Seismic cluster analysis for the Burmese–Andaman and West Sunda Arc: insight into subduction kinematics and seismic potentiality

Abstract

The Burmese–Andaman Arc System (BAAS) and the West Sunda Arc (WSA) in NE Indian Ocean are well known for their high seismic hazard and tsunami potentiality. Seismicity is caused by eastward subduction of the Indian plate to intermediate focal depths below the BAAS, but the penetration depth goes even deeper to about 500 km below the WSA. The seismicity map and its correlation to crustal and mantle faults for this extensive plate margin are presented. This is achieved by using frequency–magnitude relationship to select larger (m _b ≥ 5.0) and comparatively well-recorded events from the available earthquake catalogue that span for a period of little more than a century (1906–2008). Barely 14% of the events qualify the treatment, and the events so selected are subjected to cluster analysis using a statistical function ‘point density’. The clusters found for the arc demonstrate significant relationship to subduction geometry in their respective areas; 11 out of a total of 13 clusters commonly originate below the fore arc. Earthquakes within the individual clusters have linear fractal geometry consistent with the traces of seismogenic surfaces that actually produce them. Correlation of clusters to seismologic depth sections and the composite results derived from 518 CMT solutions of earthquakes establish a close spatial relationship between the shape and orientation of the clusters with stress axes and regional tectonics. This provides a three-dimensional perspective on the stress distribution within the respective clustered seismic zones. Seismic potentiality for five most conspicuous clusters is also inferred.

1. Introduction

The Burmese–Andaman Arc System (BAAS) and West Sunda Arc (WSA) together constitute a subducting plate margin in the NE Indian Ocean, nearly 2800 km in length, that serves as the tectonic link between the Western Pacific Arc System with the Himalayas. BAAS and the WSA have the following tectonic domains: (1) a northernmost segment of BAAS in Burma where a subduction zone is clearly discernible in a land environment delimited by Eastern Boundary Thrust (EBT); (2) further west, the trench zones of Andaman and WSA where the Indian plate subducts; (3) outer sedimentary ridge of Andaman–Nicobar–Nias Islands in between trench and the arc, followed by a continuous volcanic arc from Sumatra to Burma with active Barren Island volcano and dormant Narcondam in the central part and many dormant volcanoes in Burma; (4) Andaman back-arc spreading ridge (ASR) underlying the Andaman Sea between Alcock Rise (AR) and Sewell Rise (SR) relating to the oblique convergence of the Indian plate at the Asian continental margin in the east; actual spreading occurred through several short leaky-transforms, producing the ‘pull-apart’ Andaman basin in southern half of the BAAS; (5) further south is the intense seismic zone of the WSA with volcanism in Sumatra (figure 1). Sixteen hinge faults (figure 1) across the trend of the arc with fixed western end marked by our earlier study (Dasgupta et al. 2003) have delimited the entire study area into several blocks of individual seismic characters.

Figure 1. Tectonic domains in the Burmese–Andaman Arc System (BAAS) and the West Sunda Arc (WSA) in NE Indian Ocean. AR: Alcock Rise; ASR: Andaman Spreading Ridge; B: Barren Island volcano; BS: Belt of Shuppen; DF: Dauki Fault; EBT: Eastern Boundary Thrust; MR: Margui Ridge; N: Narcondam volcano; SR: Sewell Rise. The locations of two great earthquakes from 2004 and 2005 are shown.

The arc is unique in several ways. First is the intense seismic and tsunami hazard potentiality of the arc; the last example was the 2004 Sumatra earthquake. Seismically, the arc is not equally active throughout; a stretch of nearly 800 km between coastal Burma and the Gulf of Martaban is seismically almost passive. Second, 40% of the arc lies within the Burmese mainland where the Indian plate currently subducts to almost 200 km depth. The Neogene tectonics in central Burma is controlled by the India-Indochina oblique convergence, which is in response to a major Miocene regional plate kinematic reorganization (Bertrand and Rangin 2003). Third, the ASR underlying the Andaman Sea relates to the oblique convergence of the Indian plate at the Asian continental margin (Curray et al. 1979, Mukhopadhyay 1984). Fourth, the subduction depth in central Andaman extends to about 220 km depth (Dasgupta et al. 2003), but the subduction proceeds to about 500 km depth below the WAS further south. Fifth, the arc houses several active to dormant volcanoes, including the active Barren Island volcano in central Andaman. In the present study, our aim is to search for spatial seismic clusters in the intense seismic zones of the BAAS and WSA, in order to gain an understanding on the relationship of potential seismic clusters to structural elements of the subduction zone. In spite of more than 100 years of instrumental recording in the region (the first seismological observatory in SE Asia was established in Calcutta as early as 1897), a major limitation in the study is the non-uniform status of seismic monitoring for the arc as a whole, in particular, for the lower-magnitude shocks. This is an outcome of the typical geometric orientation of the arc, most of which lies offshore, whose remote islands locate far off from the mainland of SE Asia. These factors introduce inconsistency and incompleteness in any earthquake catalogue, resulting in inherent uncertainty in the search for ‘long-term earthquake clustering’ (Kagan and Jackson 1991), no matter what methodology is adopted. Notwithstanding these limitations, we present here an analysis of seismic clusters for the BAAS and WSA, and also investigate their respective stress characters and seismic potentiality.

2 Seismic data treatment and analysis

It is known that similar events occurring close together in space produce spatial clusters; particularly, moderate to large magnitude earthquakes often occur in spatial seismic clusters. A seismic cluster is suspected in a region if it consists of multiple events with a magnitude greater than a threshold value originating within an acceptable time period. Any statistical treatment for cluster analysis essentially therefore depends on the completeness of the earthquake catalogue (Ansari et al. 2009). The earthquake catalogue used in the present study (source: ISS, ISC and NEIC-USGS) for the BAAS and WSA consists of a total of 13,057 earthquake records for the period of 1906–2008 covering a rather wide range of magnitude (2.7 to 8.6) with focal depths extending to as deep as 500 km. Both single and cumulative earthquake frequency curves are constructed using the catalogue data. The b-value of earthquakes with m _b ≥ 4.0 calculated by the regression method is 1.0382 (figure 2(a)). Only 1752 events of magnitude 5.0 and above in the catalogue actually qualify for cluster analysis. Of these, barely 47 seismic events occurred prior to 1964, with a magnitude-frequency break-up as follows: 11 events in the magnitude range of 5.0–5.5, 20 events in the magnitude range 5.6–6.0 and 16 events of magnitude exceeding 6.0. Earthquake frequency in the lower-magnitude range (m _b = 5.0–5.5) shows a clear increase postdating 1964 (table 1) as a consequence of an increase in the number of monitoring stations. The selected events exhibit a smoother cumulative frequency curve (figure 2(b)) with a b-value of 0.9731 calculated by the regression method; this is similar to the global average of b-value of 1.0. Table 1 earthquakes, classified according to their magnitude, are superposed on a generalized tectonic map for the BAAS and WSA (figure 3).

Table 1. Earthquakes for the Andaman–Burmese arc classified according to their magnitude and frequency (used for cluster analysis).

Earthquake magnitude (m b) range	Number
5.0–5.5	1430
>5.5–6.0	241
>6.0–6.5	60
>6.5–7.0	10
>7.0	11
Total	1752

Figure 2. Frequency magnitude relationships for: (a) 13,057 events of magnitude m _b = 2.7 and above as listed in catalogue, and (b) 1752 events of m _b = 5.0 and above. The respective a are b values are given.

Figure 3. Epicentral map for the Burmese–Andaman and West Sunda Arc, period: 1906–2008. AR: Alcock Rise; ASR: Andaman Spreading Ridge; BS: Belt of Shuppen; DF: Dauki Fault; EBT: Eastern Boundary Thrust; RF: Renong Fault; SF: Semangko Fault; SR: Sewell Rise; SSF: Shan-Sagaing Fault; VA: Volcanic Arc; WAF: WEST Andaman Fault; WST: West Sundra Trench. Tectonic features are adopted after Curray et al. (1982) and Dasgupta et al. (2003).

Though several visual clusters are apparent on the map (figure 3), the following spatial statistical functionalities are applied on the dataset in table 1 to constrain their configuration and extents:

Figure 4. Seismic cluster analysis results for the Burmese–Andaman and West Sunda Arc using data plotted in figure 3. In all, 13 clusters (C1–C13) are detected; see text for discussion.

Figure 5. Frequency–magnitude distribution and fractal plots for the clustered and non-clustered events; see table 1 for their magnitude distribution.

	A point density function is applied to constrain the extent of the clusters. Point density is a classical spatial statistical tool to identify areas where data points are concentrated more or vice versa. To calculate the point density, the distance between the adjacent earthquakes is measured, and a mean distance (∼8 km) is calculated. Half of the mean distance (i.e. 4 km) is taken as the radius of the circular neighbourhood. The point density is then calculated as the total number of earthquake epicentral points that fall within a circular neighbourhood with a specific radius (in this case 4 km) divided by the area of the neighbourhood. A factor resulting from the size of the earthquake is also introduced for deriving the point density value, e.g. 6 points are counted instead 1 for an earthquake of magnitude 6 in the selected neighbourhood. This is done to offer more weight to larger earthquakes in the calculation. The measurement is then carried out in an overlapping grid pattern where the centre of the circle has been moved across the map (both along latitude and longitude) by a sliding distance of 4 km. The calculated point density value is stored in a grid point at the centre of the circle. The resulting values obtained by this sliding grid process have a mean (M) of 0.0027 and standard deviation (SD) of 0.008772. The areas with anomalous point density (value > (M + 2 SD), i.e. 0.020244) have been marked as zones of spatial clusters and shown as closed grey polygons (figure 4). This process identifies 13 numbers of spatial clusters of variable sizes with numbers C1 to C13 across the entire study area.
	Comparative statistics between clustered and non-clustered events presented in figure 5 show that almost half the population (table 1) actually originates within the cluster domains. The figure also illustrates their respective single and cumulative frequency–magnitude relationships. The ‘b’ value calculated by the regression method for the cluster zone is somewhat lower (0.8195) than that for the non-cluster zone (0.9967). However, this apparent increase in b-value is probably attributable to data inhomogeneity, rather than any true significance in data coverage for smaller-magnitude shocks.
	The geometric configuration of the clustered and non-clustered earthquakes is further constrained by fractal analysis to understand the cause–effect relationship between the occurrence of seismicity and the underlying processes that produce them. Further, once the fractal or scale-independent nature of occurrence of seismicity is established, the ‘fractal dimension’ gives the exact geometric relationship between the earthquakes points and the underlying causative surfaces. The Box-counting method (Feeder 1988) is used to calculate the fractal dimensions. The seismicity points are overlain with a grid of square boxes (pixels), which progressed from the smallest to successively larger boxes by combining the pixels in an up-scale manner (Cheng 1999). The numbers of boxes (Nn ) of size ‘rn ’ required to cover data are plotted on a log–log scale as a function of ‘rn ’. To denote the distribution as fractal, ‘Nn ’ with a characteristic linear dimension greater than ‘rn ’ must satisfy the relation Nn  = C/Nn D , where ‘C’ is the proportionality constant, and ‘D’ is the fractal dimension. ‘D' is calculated as factor log(Nn +1/Nn )/log(rn /rn +1) (Turcotte 1997). The seismicity data for both clustered and non-clustered domains (the plots of log (Nn ) versus log(1/rn )) give straight lines (right panel in figure 5). These plots indicate that the seismicity of both cases obeys scale-invariant fractal geometry, but the causative processes that generate such geometric configuration are different. The seismicity in a cluster indicates line fractal geometry with fractal dimension 1.059, whereas the non-clustered seismicity designates a point fractal geometry with fractal dimension 0.8796. This also implies that the seismicity points in clusters are arranged to form a linear pattern on the map, analogous to the traces of major seismogenic surfaces represented as a curvilinear line. Strain release by well-connected seismogenic surfaces at depth control the orientation of the clusters. On the contrary, such linear geometry is absent in case of non-clustered earthquakes with fractal dimension (0.8796), which indicates agglomeration of points. The disposition of such point fractals is not directly controlled by any seismogenic surface at depth, instead indicating sporadic strain release.

The visual relationship, thus illustrated in the foregoing section between seismic clusters and tectonic features, shows their significant distribution largely in the fore-arc for this extensive plate margin but to a much lesser extent with the ASR.

3 Discussion on cluster characteristics

3.1 Burmese Arc Clusters

Clusters C1, C2 and C3 are recognized for the Burmese Arc (figures 4 and 6(a)); these are located in north to north-central Burma in the zones of moderate seismicity. Earthquake parameters of the clusters (earthquake statistics embodied in a cluster, magnitude and depth ranges, length of the major axis) are given in table 2. Of these, cluster C2 is the largest with a maximum number of earthquakes; it is elliptical in shape with a strike length of 130 km, trends north-east and is thus sub-parallel to the local structural orientation of the arc. C1 is a small elliptical cluster in the north of Burma. C3 is a north-trending elliptical cluster located south of C2 in the same structural trend. While C2 and C3 clusters originate from the subducting Indian plate (refer to the corresponding depth sections in figures 6(c) and 6(d)), cluster C1 is from the overriding Burmese plate (figure 6(b)). None of these clusters, however, shows any association with the Burmese Volcanic Arc, which implies their tectonic origin, rather than their volcanic affinity.

Table 2. Earthquake parameters defining the clusters.

Clusters	Number of earthquakes (m b ≥ 5)	Range of m b	Depth range (km)	Length of major axis (km)
C1	11	5–6.2	9–43	58
C2	26	5–6.3	69–152	130
C3	10	5.1–5.3	60–126	64
C4	12	5–6.2	12–44	60
C5	10	5–8	20–60	55
C6	30	5–6.6	5–44	121
C7	13	5–5.3	15–39	43
C8	37	5–5.4	10–36	122
C9	225	5–6.1	3–128	324
C10	130	5–7.3	21–95	202
C11	16	5–6.1	30–68	55
C12	24	5–5.6	22–33	135
C13	343	5–8.9	1–105	460

Figure 6. (a) Tectonic map with results of CMT solutions for the three clusters, C1–C3, for the Burmese Arc. Digits refer to CMT solutions indexed in table 4. Grey circles are epicentres of earthquakes with m _b ≥5. Notice that thrust mechanisms dominate in all three clusters, where the P–T axes are orientated NE–SW and NW–SE directions. Seismological depth sections in BAAS: across the clusters (b) C1, (c) C2 and (d) C3. DF: Dauki Fault; EBT: Eastern Boundary Thrust; SF: Sagaing Fault; VA: Volcanic Arc.

The clusters C1–C3 are separated by lithospheric hinge faults, where subduction penetrates to depths of 150 km at the location of cluster C1 to 200 km at cluster C3, but then diminish to 160 km to the immediate south (Dasgupta et al. 2003). The average dip of the Benioff zone below the three clusters ranges from 42° to 50° E (figure 6). Most of the Burmese Arc seismic potentiality is therefore expected at these locales where the clusters are seen. Note that the remainder of the Burmese Arc for a distance of 1000 km up to north Andaman (where the next neighbouring clusters C4 and C5 are seen) is a cluster-free region (figure 4), as signified by its rather low level of seismicity. This is probably an outcome of passive tectonic process where the hanging lithospheric slab is being dragged northward through the surrounding lithosphere, as postulated by Le Dain et al. (1984). A somewhat analogous ‘low seismic’ region and an example of time-dependent earthquake occurrence are known for the Lower Rhine Embayment (Faenza et al. 2007).

3.2 Andaman Arc Clusters

Seismic clusters C4–C9 are located between central and south parts of the Andaman Arc (figures 4, 7(a) and 8(a)). As before, the earthquake parameters of the clusters are also indexed in table 2. All of them are shallow depth clusters but contain higher-magnitude shocks (often exceeding m _b = 6.0, sometimes as high as m _b = 8.0). Clusters C4 and C5 are located over the Andaman fore-arc (figures 7(b) and (c)), whereas cluster C6 is found at the south Andaman trench (figure 7(d)) (this is similar to cluster C12 seen for the West Sunda Trench; see below). Clusters C7 and C8 are correlated with the ASR (figures 7(a), (e) and (f)). Cluster C9 is the longest of all; it has a strike length of 324 km, contains maximum number of earthquakes and is clearly associated with the West Andaman Fault and its southern continuation to the Semangko Fault in Sumatra (figures 7(a) and (b)). The penetration depth of the subducting Indian plate in central and south Andaman extends from 130 to 220 km, where the dip of the Benioff zone varies from 30° to 45° E (Dasgupta et al. 2003). Such large variations in both the penetration depth and dip angle of the Benioff zone are typical of plate kinematics in the central and southern parts of the Andaman arc.

Figure 7. (a) Tectonic map with results of CMT solutions for clusters C4–C6 below the Andaman fore arc and clusters C7 and C8 below the ASR; see table 4 for results of the CMT solutions. Composite CMT is in the inset with grey colour circle for P axes and black circle for T axes. Other symbols are as in figure 6. Thrust mechanisms dominate in the Andaman fore arc, while normal mechanisms dominate the ASR. Notice that P–T axes are orientated E–W for the fore arc but N–S for the ASR. Seismological depth sections in BAAS: across the clusters (b) C4, (c) C5, (d) C6, (e) C7 and (f) C8. ASR: Andaman Spreading Ridge; B: Barren Volcano; N: Narcondam; SR: Sewell Rise; VA: Volcanic Arc; WAF: West Andaman Fault.

3.3 West Sunda Arc Clusters

Seismic clusters C10–C13 are seen in offshore Sumatra (figures 4 and 9(a)). As before, the earthquake parameters of the clusters are indexed in table 2. These are shallow to moderate depth clusters with a high seismicity. The configuration for all four clusters follows the structural outline of the outer sedimentary arc of the Nias and other islands. Seismically, this presents one of the most destructive regions in the world, where the 26 December 2004 Sumatra earthquake (M _w 9.3) and 2005 Banyak Island earthquake (M _w 8.7) hit. Cluster C13 is the widest of all in this zone (figure 9(a)) with a strike length of 460 km. Clusters C10 and C13 have earthquakes belonging to both plates (figures 9(b) and 9(e)), whereas cluster C11 belongs only to the overriding SE Asian plate (figure 9(c)). Cluster C12 is located below the West Sunda Trench (figure 9(d)).

Figure 8. (a) Cluster 9 skirting the Sewell Seamount, where a nascent rift was described elsewhere (Mukhopadhyay et al. 2010). Other symbols are as in figure 6. Cluster 9 typically demonstrates normal solutions for the rift, whereas strike-slip mechanisms correspond to the regional faults transverse to the rift. T axes are orientated WNW–ESE, suggesting the rifting direction perpendicular to it. (b) Seismological depth section across C9 and (c) summary plot for focal mechanism stress axes. SFS: Semangko Fault System; VA: Volcanic Arc; WAF: West Andaman Fault. The black dotted line in the depth sections traces the top of the subducting plate; the trajectories are from our earlier work (Dasgupta et al. 2003).

The present understanding on subduction kinematics for this complex arc can be improved only when a comparison of results of clustering analysis with more homogeneous data sets becomes available with a combination of greater instrumental data coverage, in particular, for smaller magnitude earthquakes. A temporary digital network established on the Andaman Islands by the Geological Survey of India recorded about 18,000 small aftershocks in about 10 weeks following the 26 December 2004 Sumatra earthquake; the recorded magnitude is 3.0 and above (Mishra et al. 2007).

4 Stress distributions and strain partitioning within seismic clusters

The Indian plate moves in a N10° E to N17° E direction between latitude 2° N (95° E longitude) and 4° N (93° E) at rates of 52 mm and 61 mm per year, respectively, beneath the Sunda Plate (Sieh and Natawidjaja 2000). The motion changes its orientation to N23° E at 9° N latitude (92° E longitude) at a rate of about 54 mm per year (DeMets et al. 1990). GPS data also indicate a non-negligible east–west convergence along the Andaman arc (Paul et al. 2001). Such differential movement vectors making a small angle to the trench axis in this oblique deformation front are partitioned between two stress components, one parallel to the trench and the other perpendicular to it. The trench parallel motion has been consumed along a large-scale crustal structure with a dominant strike-slip motion (WAF, SFS and Shan-Sagaing fault) parallel to the trench along fore-arc and also by back-arc spreading in ASR by leaky transform tectonics. The trench perpendicular component generates large-scale thrust-related motions in segments along the fore-arc (Eastern Boundary Thrust; gap between the Andaman trench and WAF, etc.).

The stress distribution and strain partitioning along different sectors have been studied in details on map and in depth sections across the clusters. Tectonic analyses of clusters are carried out with the help of composite CMT plots generated from 518 well-constrained CMT solutions collected from the HRVD website. The zone from north Burma to Sumatra has been associated with both positive and negative slips; the positive slip is accommodated primarily by thrust motion, whereas the negative slip is by normal fault or oblique slip movements. The pure strike–slip motion is in between positive and negative slips. The composite CMT plots are constructed for the clusters (figures 6 –9) distributed along the entire length of the Burmese–Andaman arc to illustrate the variation in stress axes and orientation of causative fault planes. By composite CMT plot, here we mean that all the P, T axes and pole of nodal planes of the earthquakes belonging to one cluster/multiple clusters (as the case may be) are plotted on a stereographic projection for tectonic analysis, irrespective of their type of fault plane solutions.

Figure 9. (a) Clusters C10–C13 in offshore Sumatra. This is by far the largest cluster found for the study area and is also seismically the deadliest. Other symbols are as in figure 6. Mostly thrust mechanisms prevail in the region of all four clusters, where P–T axes are orientated NE–SW. A summary plot for focal mechanism stress axes is shown in the inset. Seismological depth sections: (b) across C10 and summary plot for focal mechanism stress axes; (c) across C11; (d) across C12; and (e) seismologic section across cluster C13 of WSA, and summary plot for focal mechanism stress axes. Note the coupling between the lower and upper plates in the C10 and C13 clusters. OAR: Outer Arc Ridge; SFS: Semangko Fault system; T: Andaman Trench; VA: Volcanic Arc; WAF: West Andaman Fault.

4.1 Burmese Arc Clusters: C1–C3

CMT solutions corresponding to all three clusters found for the Burmese Arc are listed in table 3. This is a thrust-dominated domain, with subordinate strike-slip movements. Cluster C1 is a shallow focus thrust–strike-slip domain in the overriding Burma plate; C2 is an intermediate focus (>100 km) thrust-dominated domain with occasional strike–slip earthquakes along the plate interface/subducting Indian Plate. Similarly, C3 indicates a predominantly thrust domain in the subducting Indian Plate. It can also be seen that the strike-slip earthquakes within this predominantly thrust domain occur along the terminal ends of the elliptical cluster boundary. These strike slip earthquakes occur due to the movement of adjacent cross-cutting hinge faults, inferred by Dasgupta et al. (2003). Thus, the three clusters in between EBT and the volcanic arc indicate earthquake concentration predominantly along the plate interface or within plate. The CMT solution shows an overall NE–SW compression at a shallow angle (10°) and a NW–SE extension at a moderately high angle (56°) along this sector (table 4). The CMT data clearly show a dominance of thrust movement in the C2–C3 clusters with subordinate strike-slip motion both occurring even beyond a depth of 100 km; this was indicated previously by Stork et al. (2008) in the Burma subduction zone.

Table 3. CMT solutions (source: http://www.seismology.harvard.edu) for 518 earthquakes for the Burmese–Andaman and West Sunda Arc system. The solution parameters are discussed in text in relation to the seismic clusters. *Solution on the basis of Aki–Richards convention on slip. The value of first column (No) is plotted on the maps (figures 5(a)–8(a)).

No	Date	h:min:s	Latitude	Longitude	Depth	M w	T_plunge	T_azimuth	N_plunge	N_azimuth	P_plunge	P_azimuth	Plane 1 Strike	Plane 1 Dip	Plane 1 slip	Plane 2 Strike	Plane 2 Dip	Plane 2 slip	Cluster	Solution*
1	28/11/1984	10:29:29.5	26.52	96.96	16.0	5.7	38	162	47	16	18	267	311	49	17	210	77	138	C1	Strike-slip
2	7/6/2000	21:47:0.2	26.70	97.15	37.0	6.3	57	118	28	333	16	234	290	38	41	166	66	120	C1	Thrust
3	29/5/1979	0:39:55.7	24.92	95.05	108.5	5.4	60	120	20	250	21	348	109	30	134	241	69	68	C2	Thrust
4	23/8/1983	12:12:19	24.48	94.69	147.9	5.2	67	127	22	321	5	229	297	44	58	158	54	118	C2	Thrust
5	13/8/1988	19:59:52.7	24.94	95.24	126.0	5.1	73	98	12	325	12	232	307	35	69	152	58	104	C2	Thrust
6	9/1/1990	18:51:36.2	24.42	94.95	129.6	6.3	58	142	24	276	20	16	140	32	139	267	69	64	C2	Thrust
7	8/8/1994	21:8:36.6	24.76	94.97	145.6	6.1	68	129	16	266	14	0	111	34	120	257	61	71	C2	Thrust
8	6/5/1995	1:59:13.8	24.83	95.02	147.7	6.4	69	94	19	302	9	209	278	39	60	135	57	112	C2	Thrust
9	2/5/1998	8:36:54.6	24.84	95.09	127.4	5.5	32	92	58	271	0	2	132	68	156	232	68	24	C2	Strike-slip
10	2/7/2000	4:27:58	24.45	94.67	103.2	5.2	48	117	33	254	22	359	133	37	155	244	75	56	C2	Thrust
11	12/8/2001	1:58:0.9	24.43	94.99	142.0	5.1	62	112	26	320	12	224	285	40	48	155	61	119	C2	Thrust
12	15/2/2005	13:5:53.8	24.40	94.62	60.4	5.2	40	132	50	318	3	225	276	61	28	171	65	147	C2	Strike-slip
13	18/9/2005	7:26:1.7	24.48	94.71	105.4	5.7	50	121	40	308	3	215	271	54	38	156	60	138	C2	Strike-slip
14	1/5/1981	4:8:13	23.32	94.64	99.1	5.0	49	70	21	314	34	210	247	22	21	137	82	111	C3	Thrust
15	24/8/1987	9:24:44.4	23.04	94.53	126.5	5.3	54	119	33	270	14	9	135	42	144	254	67	54	C3	Thrust
16	11/10/2000	9:42:11.1	23.58	94.63	122.3	5.6	58	62	2	155	31	246	343	14	98	155	77	88	C3	Thrust
17	7/5/2007	5:58:36.7	23.02	94.58	97.3	5.0	24	90	66	285	5	183	229	69	13	134	77	159	C3	Strike-slip
18	7/12/2007	6:56:33	23.46	94.66	108.7	5.0	69	131	20	292	6	24	135	42	120	277	54	65	C3	Thrust
19	7/2/1978	12:30:48.2	12.98	93.19	15.0	5.6	60	321	28	164	10	69	129	43	46	2	61	123	C4	Thrust
20	7/2/1978	20:32:1	12.83	93.03	15.0	5.7	81	230	3	338	9	68	162	36	95	336	54	86	C4	Thrust
21	20/9/1986	10:4:58.7	12.82	93.16	21.6	5.1	62	114	12	1	25	266	332	23	59	185	71	102	C4	Thrust
22	20/11/2003	00:14:5:4	13.21	93.07	39.2	5.4	66	173	21	22	11	288	354	39	55	216	59	115	C4	Thrust
23	6/3/2004	10:21:34.4	13.05	93.19	24.7	5.5	41	184	46	339	13	82	214	52	157	319	72	41	C4	Strike-slip
24	10/4/2004	15:57:4	13.19	93.09	33.4	5.1	72	129	8	14	16	281	359	30	73	198	62	99	C4	Thrust
25	3/5/2004	17:41:32.5	13.18	93.19	27.8	5.2	72	151	12	20	13	287	1	34	68	207	59	104	C4	Thrust
26	29/1/2005	5:44:13.6	13.18	93.07	20.6	5.2	58	314	30	155	9	59	118	44	44	353	61	125	C4	Thrust
27	30/1/2005	7:2:25.1	13.20	92.97	23.1	5.1	24	324	65	158	5	56	103	69	14	8	77	158	C4	Strike-slip
28	21/1/2006	4:7:7	13.10	93.23	39.0	5.7	72	77	6	187	17	279	19	29	103	184	62	83	C4	Thrust
29	27/12/2004	14:46:48.6	12.39	92.72	27.0	5.6	28	81	8	346	61	242	191	19	−64	344	73	−98	C5	Normal
30	4/1/2005	9:13:17.4	10.65	92.03	24.0	6.0	64	68	6	170	25	263	5	20	107	168	70	84	C6	Thrust
31	28/12/2004	10:51:50.6	10.61	92.20	12.0	5.3	51	66	5	162	39	257	22	8	130	162	84	85	C6	Thrust
32	28/12/2004	23:40:2.1	11.12	92.04	12.0	5.0	6	276	29	9	61	174	337	46	−132	209	57	−55	C6	Normal
33	31/12/2004	5:53:57	11.15	91.98	12.5	5.1	13	316	40	57	47	212	7	48	−151	256	69	−46	C6	Normal
34	1/1/2005	11:53:14.1	11.14	91.67	21.6	5.0	9	287	13	19	74	162	1	37	−112	208	56	−74	C6	Normal
35	6/1/2005	11:55:47.8	11.01	91.99	13.0	5.5	23	92	17	354	61	232	211	26	−50	348	70	−108	C6	Normal
36	27/1/2005	5:51:4.4	10.72	91.72	37.3	5.2	77	7	13	188	0	98	175	46	72	20	47	108	C6	Thrust
37	22/2/2005	17:12:1.5	10.81	91.72	12.0	5.5	70	121	10	3	18	270	345	29	69	188	63	101	C6	Thrust
38	10/4/2005	2:23:51.4	10.75	92.09	12.0	5.0	52	78	11	182	36	280	56	13	144	181	82	79	C6	Thrust
39	22/12/2006	19:50:49	10.70	92.11	22.0	6.2	59	73	1	165	31	255	350	14	95	164	76	89	C6	Thrust
40	29/8/2005	14:44:48.8	11.04	91.92	21.0	5.2	60	100	7	357	28	263	334	18	66	179	74	97	C6	Thrust
41	11/10/2005	3:38:0.9	10.89	92.02	24.0	5.3	66	71	4	171	23	263	1	22	101	169	68	86	C6	Thrust
42	5/2/2006	13:40:35.8	11.03	91.75	15.8	4.8	10	277	6	8	79	129	359	36	−100	192	55	−83	C6	Normal
43	9/6/1991	20:39:36.5	12.70	95.14	40.6	5.5	2	332	87	116	2	242	17	87	180	107	90	3	C7	Strike-slip
44	19/3/1993	15:53:57.6	12.62	95.75	15.0	5.3	0	129	30	219	60	38	192	52	−129	65	52	−51	C7	Normal
45	13/1/2003	16:35:1.9	12.93	95.65	15.0	5.3	25	332	52	100	26	229	11	52	−180	281	90	−38	C7	Strike-slip
46	26/1/2003	10:49:30.4	12.98	95.36	26.0	5.1	34	97	32	342	40	220	245	32	−6	340	87	−122	C7	Normal
47	19/7/1984	16:16:10.6	11.11	94.58	25.1	4.8	2	344	23	253	67	79	96	47	−58	233	52	−120	C8	Normal
48	10/3/2006	4:5:44.3	10.73	94.37	12.0	5.5	11	338	2	69	79	170	66	34	−94	250	56	−87	C8	Normal
49	10/3/2006	4:43:35.4	10.64	94.35	12.0	5.2	11	330	1	60	79	155	59	34	−92	241	56	−89	C8	Normal
50	10/3/2006	5:6:12	10.69	94.41	12.0	5.1	15	333	16	67	68	200	41	33	−120	255	62	−72	C8	Normal
51	10/3/2006	12:4:0.3	10.79	94.53	12.0	5.2	16	344	3	75	73	174	70	29	−96	256	61	−87	C8	Normal
52	11/3/2006	11:48:53.1	10.69	94.40	12.0	5.1	1	321	11	52	79	225	40	45	−106	242	47	−74	C8	Normal
53	16/3/2006	13:59:23.8	10.75	94.45	12.0	5.5	11	342	0	72	79	164	71	34	−91	252	56	−90	C8	Normal
54	19/3/2006	19:12:16.2	10.78	94.52	12.0	4.9	12	344	3	253	77	148	78	33	−84	251	57	−94	C8	Normal
55	19/3/2006	21:57:16.6	10.77	94.46	12.0	5.0	11	349	6	258	78	142	86	35	−80	254	56	−97	C8	Normal
56	9/8/1994	23:35:1.7	10.57	94.34	33.0	5.5	28	339	11	243	60	133	96	20	−55	239	74	−102	C8	Normal
57	10/8/1994	1:39:29.7	10.96	94.35	15.0	5.4	0	142	2	52	88	232	234	45	−87	49	45	−93	C8	Normal
58	9/3/2006	14:48:56.8	10.79	94.48	12.0	4.9	12	343	10	251	74	124	85	34	−73	245	58	−101	C8	Normal
59	9/3/2006	14:57:12.4	10.80	94.14	12.0	5.1	40	291	6	196	50	99	63	8	−43	196	85	−96	C8	Normal
60	9/3/2006	15:3:16	10.87	94.55	17.1	5.1	10	340	9	72	76	203	58	36	−106	258	56	−79	C8	Normal
61	9/3/2006	15:12:4.4	10.78	94.51	12.0	5.2	13	337	17	243	68	101	89	36	−59	232	60	−110	C8	Normal
62	9/3/2006	15:19:18.6	10.89	94.68	12.0	5.2	14	344	10	76	73	199	60	32	−108	262	60	−79	C8	Normal
63	9/3/2006	15:46:58.6	10.81	94.49	12.0	5.0	11	347	5	256	78	140	83	35	−81	252	56	−96	C8	Normal
64	9/3/2006	16:42:37.4	10.73	94.48	21.4	5.0	2	347	4	77	86	230	74	43	−95	261	47	−85	C8	Normal
65	9/3/2006	17:9:10.1	10.83	94.47	18.2	5.0	10	331	6	240	78	118	69	36	−79	235	55	−98	C8	Normal
66	9/3/2006	18:21:55.4	10.82	94.69	12.0	5.4	6	347	4	257	83	137	81	39	−84	254	52	−95	C8	Normal
67	9/3/2006	18:26:33.1	10.79	94.51	12.0	5.3	25	344	20	244	57	121	111	27	−40	238	73	−111	C8	Normal
68	9/3/2006	19:15:46	10.79	94.55	12.1	5.2	6	346	4	77	83	199	72	39	−96	260	51	−85	C8	Normal
69	9/3/2006	20:25:47.7	10.79	94.52	12.0	5.2	20	347	10	80	67	195	60	26	−113	265	66	−79	C8	Normal
70	9/3/2006	21:18:57.7	10.86	94.66	12.0	5.0	15	344	4	253	75	148	79	31	−82	250	60	−94	C8	Normal
71	9/3/2006	21:37:2.4	10.76	94.49	12.0	5.3	10	346	7	77	77	203	67	36	−103	263	56	−81	C8	Normal
72	9/3/2006	22:30:49	10.75	94.46	12.0	5.3	13	346	0	255	77	164	76	32	−90	255	58	−90	C8	Normal
73	10/3/2006	1:13:43.8	10.72	94.67	18.1	4.9	20	156	12	61	67	302	266	28	−63	56	66	−103	C8	Normal
74	8/6/1979	20:36:41.4	7.47	94.14	124.3	5.1	58	163	3	68	32	336	55	13	77	249	77	93	C9	Thrust
75	8/4/1982	21:34:19	7.40	94.10	33.0	5.3	8	306	79	170	8	37	81	79	0	351	90	169	C9	Strike-slip
76	22/5/1982	8:53:4.8	7.61	94.39	12.2	5.5	23	296	3	27	67	125	19	23	−98	208	68	−86	C9	Normal
77	28/1/1986	12:32:18.6	8.81	94.01	15.0	6.0	2	301	86	55	4	211	346	86	−178	256	88	−4	C9	Strike-slip
78	19/6/1986	18:12:32.8	7.90	94.40	181.3	5.9	23	204	18	302	60	66	263	27	−132	128	70	−71	C9	Normal
79	19/2/1989	1:46:1.6	7.65	94.47	15.0	5.3	17	95	57	212	27	356	138	58	−172	43	83	−32	C9	Strike-slip
80	30/4/1990	18:0:25.6	8.05	94.50	15.0	5.6	10	288	73	55	13	195	332	73	−178	241	88	−17	C9	Strike-slip
81	18/8/1990	18:52:43.3	7.75	93.86	15.0	6.0	12	141	73	275	11	48	185	73	180	275	90	17	C9	Strike-slip
82	29/12/1990	13:23:55.2	8.14	93.93	21.0	6.1	3	302	86	90	2	212	347	86	179	77	89	4	C9	Strike-slip
83	18/7/1991	9:50:41.6	8.37	94.29	41.9	5.5	3	297	87	137	1	28	73	87	1	342	89	177	C9	Strike-slip
84	26/8/1991	20:54:25.4	7.30	94.54	49.6	5.9	5	281	67	24	22	189	327	71	−168	233	78	−20	C9	Strike-slip
85	4/1/2005	12:15:36	8.83	93.64	12.0	4.9	26	127	7	221	62	325	199	20	−112	43	72	−82	C9	Normal
86	25/5/1994	18:42:23.6	7.70	94.37	41.4	5.9	6	103	84	272	1	13	148	85	177	238	87	5	C9	Strike-slip
87	27/7/1995	15:16:32.8	9.18	93.97	26.7	5.2	4	145	54	241	36	52	195	62	−156	93	69	−30	C9	Strike-slip
88	13/4/1996	10:45:22.4	7.28	94.57	48.1	5.4	2	101	87	223	3	11	146	87	−179	56	89	−3	C9	Strike-slip
89	25/6/1996	7:28:59.1	8.65	93.87	29.9	5.2	6	306	83	140	2	37	82	84	3	351	87	174	C9	Strike-slip
90	12/1/1998	22:40:2.3	9.38	93.63	110.8	5.4	42	75	48	252	2	344	111	60	149	218	64	33	C9	Strike-slip
91	9/8/1998	0:34:58.2	7.43	94.42	28.0	5.4	12	104	77	291	1	195	240	80	8	149	82	170	C9	Strike-slip
92	10/8/1998	9:52:17.5	7.58	94.39	23.7	5.9	5	102	84	326	4	192	237	84	0	147	90	174	C9	Strike-slip
93	15/10/1998	19:5:26.6	7.73	94.34	52.1	5.4	8	112	78	244	8	21	156	78	−180	66	90	−12	C9	Strike-slip
94	29/8/1999	3:44:51.6	8.88	93.52	24.8	5.2	31	151	55	301	14	52	187	58	167	285	79	33	C9	Strike-slip
95	18/12/1999	0:50:33.5	7.05	94.56	25.0	5.2	13	278	67	156	19	12	54	67	−5	146	85	−157	C9	Strike-slip
96	15/3/2001	0:39:11	8.76	94.08	28.3	5.4	5	115	81	355	8	206	250	81	−2	341	88	−171	C9	Strike-slip
97	15/3/2001	1:22:44.3	8.79	94.11	29.9	6.0	5	303	81	65	8	213	348	81	−178	258	88	−9	C9	Strike-slip
98	17/1/2003	14:31:12.7	8.00	93.89	17.1	5.2	9	135	69	20	19	229	271	70	−7	3	84	−160	C9	Strike-slip
99	30/1/2003	17:21:9.4	7.80	94.32	37.1	5.2	1	102	83	6	7	192	237	85	−5	327	85	−174	C9	Strike-slip
100	15/4/2004	21:20:42	8.80	94.10	18.6	5.3	12	113	78	285	2	23	157	80	173	249	83	10	C9	Strike-slip
101	15/4/2004	23:2:15	8.85	94.15	17.6	5.0	21	117	36	223	47	3	163	40	−156	54	75	−53	C9	Normal
102	16/4/2004	2:6:15.3	8.88	94.14	21.1	5.6	4	110	76	218	13	19	156	78	−174	64	84	−12	C9	Strike-slip
103	16/4/2004	11:29:48.7	8.90	94.05	22.5	4.8	15	106	72	251	10	13	149	72	176	240	86	18	C9	Strike-slip
104	18/5/2004	2:58:18.7	7.40	93.81	73.3	5.0	20	87	70	267	0	177	223	76	14	130	76	165	C9	Strike-slip
105	26/12/2004	10:18:14.6	8.91	94.11	33.3	6.4	72	279	16	73	7	165	272	40	115	61	54	70	C9	Thrust
106	27/12/2004	0:39:46.9	8.98	93.69	15.8	5.4	3	105	22	196	68	6	173	46	−121	34	52	−62	C9	Normal
107	11/1/2005	5:49:31.6	8.16	93.85	12.9	4.9	5	307	18	39	71	202	19	43	−117	233	53	−67	C9	Normal
108	27/12/2004	2:4:25.6	8.07	94.29	12.0	5.2	27	86	29	339	48	211	223	32	−23	333	78	−120	C9	Normal
109	27/12/2004	14:30:36.3	8.63	93.90	12.0	5.2	25	79	31	333	48	201	215	34	−23	325	77	−122	C9	Normal
110	27/12/2004	19:28:53.3	8.72	93.93	12.0	5.3	21	78	5	346	68	245	177	24	−79	344	66	−95	C9	Normal
111	27/12/2004	20:36:19.8	8.93	93.80	12.0	5.3	15	83	4	352	74	249	178	30	−83	350	60	−94	C9	Normal
112	28/12/2004	0:37:53.5	7.61	94.32	22.0	5.5	1	97	80	193	10	7	143	82	−174	52	84	−8	C9	Strike-slip
113	28/12/2004	5:36:14.3	9.48	93.77	12.0	5.4	9	98	9	7	77	232	199	37	−74	0	55	−101	C9	Normal
114	28/12/2004	19:55:12.9	9.44	93.76	12.0	5.2	8	99	8	8	78	231	199	38	−76	1	54	−101	C9	Normal
115	28/12/2004	21:47:33	9.06	93.78	12.0	5.4	14	87	23	351	62	205	205	37	−49	338	63	−116	C9	Normal
116	29/12/2004	1:50:57.7	9.12	93.97	12.0	6.0	11	99	28	4	60	208	220	42	−46	347	61	−122	C9	Normal
117	29/12/2004	6:19:7	9.55	93.90	12.0	5.4	18	99	14	4	67	239	210	30	−61	358	64	−105	C9	Normal
118	29/12/2004	10:9:23.8	7.61	93.81	12.0	5.0	3	339	22	70	67	242	47	46	−122	269	52	−61	C9	Normal
119	29/12/2004	22:55:44.6	7.67	93.78	19.6	4.8	1	348	1	258	89	117	79	44	−89	257	46	−91	C9	Normal
120	31/12/2004	9:57:4.2	7.62	94.00	12.0	5.6	6	297	30	30	59	197	358	47	−133	232	58	−53	C9	Normal
121	31/12/2004	16:15:47.7	7.56	93.99	12.0	4.9	8	109	1	199	82	297	197	37	−92	20	53	−89	C9	Normal
122	1/1/2005	1:42:23.8	7.24	93.96	12.0	5.0	16	149	43	44	43	254	282	48	−23	28	73	−136	C9	Strike-slip
123	1/1/2005	19:8:5.8	7.15	94.49	19.8	6.1	0	290	72	199	18	20	63	77	−13	156	78	−167	C9	Strike-slip
124	7/1/2005	10:49:15.2	8.89	93.61	12.0	5.3	1	108	21	17	69	200	218	48	−61	358	50	−119	C9	Normal
125	18/1/2005	22:4:46.7	8.34	93.97	26.1	4.9	1	128	80	222	10	38	173	82	−173	82	83	−8	C9	Strike-slip
126	26/1/2005	17:30:30.4	8.20	94.14	12.0	5.6	1	117	63	209	27	27	165	71	−161	69	72	−20	C9	Strike-slip
127	26/1/2005	22:47:0.6	7.92	94.14	21.4	5.5	14	114	70	246	14	20	157	70	−180	67	90	−20	C9	Strike-slip
128	26/1/2005	23:3:8.6	7.94	94.23	14.6	5.1	22	111	32	215	49	353	158	37	−153	46	74	−56	C9	Normal
129	27/1/2005	3:58:45.6	7.94	94.20	19.5	5.4	16	111	64	236	21	15	154	64	−176	62	87	−26	C9	Strike-slip
130	27/1/2005	4:2:50.1	7.89	94.21	12.7	5.1	27	106	49	233	28	1	144	49	−179	53	89	−41	C9	Strike-slip
131	27/1/2005	5:22:20.3	7.90	94.18	19.7	5.4	13	111	65	231	21	16	155	65	−174	62	85	−25	C9	Strike-slip
132	27/1/2005	5:48:12.9	7.99	94.20	14.9	5.3	27	112	48	236	30	6	150	48	−177	58	88	−42	C9	Strike-slip
133	27/1/2005	6:14:31	7.94	94.18	12.0	5.0	21	100	34	205	49	345	148	39	−153	36	74	−54	C9	Normal
134	27/1/2005	6:56:58.6	7.92	94.17	18.5	5.6	2	120	75	219	15	30	166	78	−171	74	81	−12	C9	Strike-slip
135	27/1/2005	7:20:26.4	7.95	94.19	14.0	5.2	21	114	38	221	45	2	159	41	−158	52	75	−51	C9	Normal
136	27/1/2005	7:26:1.8	7.99	94.21	21.6	5.3	21	112	62	248	18	15	153	62	178	244	88	28	C9	Strike-slip
137	27/1/2005	7:28:32.2	7.98	94.22	22.9	5.2	3	311	38	43	52	218	9	54	−139	252	58	−44	C9	Strike-slip
138	27/1/2005	7:35:46.9	7.96	94.20	17.0	5.2	11	124	75	346	9	216	260	76	1	170	89	166	C9	Strike-slip
139	27/1/2005	7:41:26.2	7.90	94.25	22.2	4.9	19	100	58	223	25	1	142	58	−175	50	86	−32	C9	Strike-slip
140	27/1/2005	8:7:26.3	7.93	94.20	14.2	5.2	14	125	51	234	35	25	170	55	−164	71	77	−37	C9	Strike-slip
141	27/1/2005	8:19:9.1	7.93	94.17	12.0	5.5	3	124	83	239	7	33	168	83	−178	78	88	−7	C9	Strike-slip
142	27/1/2005	8:31:12.1	7.96	94.22	14.6	5.3	12	95	75	235	9	3	138	75	178	229	88	15	C9	Strike-slip
143	27/1/2005	8:36:52	7.89	94.21	16.5	5.2	29	125	35	238	41	6	162	36	−169	63	83	−55	C9	Normal
144	27/1/2005	8:42:16.1	7.83	94.22	14.8	5.5	24	106	51	229	29	1	145	51	−176	53	87	−39	C9	Strike-slip
145	27/1/2005	9:11:28.8	8.11	94.26	16.1	5.2	17	108	37	5	48	218	240	43	−27	350	72	−129	C9	Normal
146	27/1/2005	9:25:28.7	7.94	94.16	17.7	5.2	16	129	60	251	24	32	172	61	−174	79	85	−29	C9	Strike-slip
147	27/1/2005	9:52:21.3	7.87	94.25	20.0	5.4	19	102	65	241	15	7	144	65	177	235	87	25	C9	Strike-slip
148	27/1/2005	9:59:31.8	7.98	94.22	25.2	5.3	12	125	65	243	22	30	169	66	−173	76	84	−25	C9	Strike-slip
149	27/1/2005	10:8:13.5	7.92	94.16	19.5	5.3	14	117	50	224	36	16	163	54	−162	62	76	−37	C9	Strike-slip
150	27/1/2005	10:25:53.7	7.99	94.26	12.0	5.1	26	102	41	217	38	349	141	42	−169	43	83	−49	C9	Normal
151	27/1/2005	10:58:7.5	7.91	94.11	13.9	5.3	0	129	90	295	0	39	174	90	180	264	90	0	C9	Strike-slip
152	27/1/2005	11:44:6.3	8.02	94.15	12.0	5.3	4	118	48	23	42	212	246	58	−29	353	65	−145	C9	Strike-slip
153	27/1/2005	11:47:36.9	7.92	94.20	12.0	5.5	3	301	86	160	2	31	76	86	0	346	90	176	C9	Strike-slip
154	27/1/2005	11:56:43.5	7.88	94.16	15.5	5.1	16	127	30	226	55	12	181	39	−143	60	67	−57	C9	Normal
155	27/1/2005	12:11:55.3	7.98	94.28	12.0	5.4	4	139	86	295	2	49	184	86	178	274	88	4	C9	Strike-slip
156	27/1/2005	13:15:20.4	7.86	94.14	17.1	5.4	18	110	61	235	22	12	152	61	−177	60	87	−29	C9	Strike-slip
157	27/1/2005	13:18:5.7	7.92	94.25	23.3	5.3	15	104	61	223	24	8	148	62	−173	55	84	−28	C9	Strike-slip
158	27/1/2005	13:25:21.6	7.77	94.20	18.1	5.2	16	108	69	245	13	14	150	69	178	241	88	21	C9	Strike-slip
159	27/1/2005	13:26:33.6	7.84	94.24	22.2	5.3	18	112	67	252	14	18	154	67	177	245	87	23	C9	Strike-slip
160	27/1/2005	13:54:15.4	7.92	94.17	19.5	5.4	5	121	79	240	10	30	166	79	−177	76	87	−11	C9	Strike-slip
161	27/1/2005	13:57:7.2	7.97	94.16	16.3	5.5	9	110	65	221	23	16	155	67	−170	62	81	−23	C9	Strike-slip
162	27/1/2005	14:13:18	7.95	94.14	17.3	5.1	22	107	30	211	51	347	155	35	−151	41	74	−58	C9	Normal
163	27/1/2005	14:35:9.2	7.95	94.20	22.3	5.1	16	117	61	239	23	20	160	62	−175	67	85	−28	C9	Strike-slip
164	27/1/2005	15:24:51.5	7.66	94.21	24.7	5.2	23	129	50	8	31	233	268	51	−6	2	85	−140	C9	Strike-slip
165	27/1/2005	15:27:53.8	7.94	94.16	12.0	5.3	11	129	57	22	31	226	263	61	−15	1	77	−150	C9	Strike-slip
166	27/1/2005	15:34:30.4	7.74	94.25	23.0	5.3	11	113	45	215	43	13	163	52	−154	56	70	−41	C9	Strike-slip
167	27/1/2005	16:0:57.9	7.76	94.18	32.5	5.0	31	123	59	294	4	31	162	66	160	261	72	25	C9	Strike-slip
168	27/1/2005	16:2:22.3	8.04	94.25	31.6	5.1	5	126	77	237	12	35	171	78	−175	80	85	−12	C9	Strike-slip
169	27/1/2005	16:48:28.5	7.94	94.14	12.0	5.0	4	306	81	187	8	37	81	82	−2	171	88	−172	C9	Strike-slip
170	27/1/2005	16:58:52.3	7.81	94.24	19.5	5.8	4	104	77	212	12	13	149	78	−174	58	84	−12	C9	Strike-slip
171	27/1/2005	17:25:1.9	7.78	94.25	19.0	5.4	20	115	62	250	18	18	156	62	178	247	88	28	C9	Strike-slip
172	27/1/2005	17:40:49.5	7.92	94.17	13.0	5.4	13	121	20	216	66	360	187	36	−125	48	61	−67	C9	Normal
173	27/1/2005	18:52:39.3	7.85	94.24	15.9	5.6	13	102	64	220	22	7	146	65	−173	53	84	−25	C9	Strike-slip
174	27/1/2005	19:20:21.9	7.91	94.17	12.0	5.3	8	123	23	216	66	16	189	42	−125	52	56	−63	C9	Normal
175	27/1/2005	19:31:11.1	8.00	94.20	19.3	5.2	13	115	42	216	45	12	165	49	−152	56	69	−45	C9	Normal
176	27/1/2005	19:40:39.5	8.16	94.07	15.3	5.3	13	133	17	227	68	9	202	36	−121	58	60	−70	C9	Normal
177	27/1/2005	20:17:39.2	8.01	94.19	22.6	5.1	13	114	55	223	32	16	159	58	−165	62	78	−33	C9	Strike-slip
178	27/1/2005	20:31:2.8	7.97	94.19	16.3	5.2	19	120	36	224	48	7	167	41	−153	57	73	−52	C9	Normal
179	27/1/2005	20:45:20.1	7.89	94.19	15.1	5.0	24	137	20	236	58	1	191	27	−138	63	72	−69	C9	Normal
180	27/1/2005	20:51:10.9	8.11	94.18	16.6	5.2	0	138	78	231	12	48	184	81	−172	93	82	−9	C9	Strike-slip
181	27/1/2005	21:5:5.3	7.99	94.26	15.4	5.1	25	86	49	208	30	340	125	49	−176	32	87	−41	C9	Strike-slip
182	27/1/2005	21:32:20	7.98	94.17	17.0	5.2	13	108	53	215	34	9	154	57	−163	54	76	−34	C9	Strike-slip
183	27/1/2005	21:47:56.1	7.95	94.17	12.0	5.2	18	121	0	211	72	301	211	27	−90	31	63	−90	C9	Normal
184	27/1/2005	22:40:48.4	8.00	94.18	12.0	5.4	5	122	23	30	66	223	235	45	−56	12	54	−119	C9	Normal
185	27/1/2005	22:56:51.4	8.05	94.31	21.9	5.0	16	117	32	217	54	4	170	40	−145	52	68	−56	C9	Normal
186	27/1/2005	23:20:9.1	8.02	94.20	12.0	5.4	15	110	49	218	36	8	155	53	−163	54	77	−39	C9	Strike-slip
187	27/1/2005	23:27:3.2	7.89	94.23	22.8	5.1	35	106	54	268	9	10	142	60	160	243	73	32	C9	Strike-slip
188	27/1/2005	23:40:49.5	8.00	94.25	21.6	4.9	8	108	34	204	55	7	166	47	−139	45	61	−51	C9	Normal
189	28/1/2005	0:15:46.5	7.84	94.21	17.6	5.3	16	111	62	233	23	14	154	62	−175	62	85	−28	C9	Strike-slip
190	28/1/2005	1:1:29.6	7.94	94.17	12.0	4.9	6	128	19	221	70	22	198	42	−119	55	54	−66	C9	Normal
191	28/1/2005	1:36:20.2	7.96	94.23	12.0	5.2	18	123	6	215	71	322	204	27	−102	38	63	−84	C9	Normal
192	28/1/2005	1:43:39.8	7.96	94.23	28.2	5.0	9	117	4	208	80	325	202	37	−97	31	54	−85	C9	Normal
193	28/1/2005	2:23:15.6	7.87	94.20	15.5	5.3	18	100	46	210	38	355	144	48	−163	43	78	−43	C9	Strike-slip
194	28/1/2005	2:28:58.3	7.99	94.15	12.0	5.2	15	117	29	18	56	231	241	39	−39	4	66	−122	C9	Normal
195	28/1/2005	3:31:26.9	8.06	94.20	12.0	5.4	1	123	35	33	55	215	244	54	−45	4	56	−134	C9	Normal
196	28/1/2005	4:34:41.6	7.89	94.23	17.6	5.2	29	128	53	265	21	26	164	54	174	258	85	37	C9	Strike-slip
197	28/1/2005	5:4:34.6	7.88	94.18	12.0	5.4	15	100	59	215	27	2	144	60	−170	49	82	−30	C9	Strike-slip
198	28/1/2005	5:38:27.1	7.82	94.20	17.4	5.1	20	106	48	220	35	2	149	50	−168	51	81	−41	C9	Strike-slip
199	28/1/2005	6:6:55.5	7.73	94.21	16.8	5.4	0	262	52	172	38	353	31	64	−29	134	65	−151	C9	Strike-slip
200	28/1/2005	6:10:30.1	7.85	94.17	12.0	5.5	15	99	59	215	27	2	143	60	−171	49	82	−30	C9	Strike-slip
201	28/1/2005	6:13:27.6	7.79	94.16	17.8	5.7	9	106	64	215	24	12	152	66	−168	57	79	−24	C9	Strike-slip
202	28/1/2005	7:49:17.5	7.82	94.23	16.0	5.6	13	98	58	210	29	1	143	60	−168	47	80	−30	C9	Strike-slip
203	28/1/2005	8:21:23.9	8.01	94.17	12.0	5.3	9	121	5	30	80	270	217	37	−82	27	54	−96	C9	Normal
204	28/1/2005	8:29:47.2	7.82	94.27	18.4	5.3	20	102	41	211	42	353	147	44	−161	43	77	−48	C9	Normal
205	28/1/2005	8:47:18.7	7.84	94.11	13.1	5.3	23	103	55	228	26	1	143	55	−177	51	88	−35	C9	Strike-slip
206	28/1/2005	9:14:46.4	8.00	94.21	22.0	5.2	17	118	63	244	20	21	160	63	−177	69	88	−27	C9	Strike-slip
207	28/1/2005	10:21:20.5	7.66	93.91	19.4	5.2	17	277	31	176	53	31	45	39	−34	163	69	−124	C9	Normal
208	28/1/2005	11:53:3.7	7.84	94.23	17.2	5.3	10	100	65	212	23	5	145	67	−170	51	81	−24	C9	Strike-slip
209	28/1/2005	12:37:13.2	8.07	94.22	12.0	5.1	5	122	21	30	69	225	233	44	−60	14	53	−116	C9	Normal
210	28/1/2005	17:49:41.5	8.12	94.30	12.0	5.1	15	113	11	20	71	256	219	31	−68	14	61	−103	C9	Normal
211	28/1/2005	19:18:54.6	7.86	94.20	12.0	5.5	12	98	59	208	28	1	143	61	−167	47	79	−29	C9	Strike-slip
212	28/1/2005	22:29:4.4	7.75	94.23	20.6	5.4	17	113	68	253	13	19	155	68	177	246	87	22	C9	Strike-slip
213	28/1/2005	22:35:29.5	7.71	94.01	15.3	5.2	18	109	17	13	65	242	224	31	−55	5	65	−109	C9	Normal
214	28/1/2005	23:32:11.8	8.05	94.24	12.0	5.0	7	119	17	27	71	229	228	41	−63	14	54	−112	C9	Normal
215	29/1/2005	1:50:22.1	7.77	94.23	21.3	5.4	4	114	80	227	9	23	159	81	−176	68	86	−9	C9	Strike-slip
216	29/1/2005	3:38:3.6	8.09	94.25	12.0	5.1	10	117	19	24	68	233	229	39	−59	11	58	−113	C9	Normal
217	29/1/2005	5:26:48.8	7.82	94.20	12.0	5.3	15	99	63	221	22	3	142	64	−175	50	85	−26	C9	Strike-slip
218	29/1/2005	9:27:40.1	7.76	94.29	15.4	5.0	22	108	51	229	30	4	148	52	−174	54	85	−38	C9	Strike-slip
219	29/1/2005	16:12:50.9	8.18	94.25	25.4	5.0	17	109	61	231	23	11	151	61	−175	59	86	−29	C9	Strike-slip
220	29/1/2005	16:36:55.6	8.05	94.26	12.0	5.1	13	113	15	19	70	242	222	35	−63	10	60	−108	C9	Normal
221	29/1/2005	18:37:58.4	8.11	94.33	15.6	4.9	4	119	28	27	62	217	236	48	−51	5	55	−125	C9	Normal
222	29/1/2005	19:6:16.5	7.72	94.29	15.1	5.3	14	90	61	206	25	353	134	62	−171	40	82	−28	C9	Strike-slip
223	29/1/2005	20:1:57.7	8.10	94.22	12.0	5.3	2	117	42	26	48	209	242	57	−37	354	60	−141	C9	Strike-slip
224	29/1/2005	20:28:24.5	7.75	94.21	19.0	5.6	6	109	74	220	15	18	154	75	−174	63	84	−15	C9	Strike-slip
225	29/1/2005	20:54:26	7.82	94.20	12.4	5.0	30	107	31	217	45	342	145	32	−164	42	82	−59	C9	Normal
226	29/1/2005	20:58:34.6	8.01	94.19	12.0	5.0	17	126	3	217	73	316	211	28	−96	38	62	−87	C9	Normal
227	29/1/2005	22:3:52.6	7.80	94.18	12.0	5.4	7	100	64	204	25	6	146	67	−167	51	78	−23	C9	Strike-slip
228	30/1/2005	0:7:35	8.13	94.21	19.7	5.3	1	130	75	223	15	39	176	79	−170	84	80	−11	C9	Strike-slip
229	30/1/2005	0:34:11.4	8.07	94.21	13.6	5.1	5	125	32	31	57	223	245	49	−45	8	58	−129	C9	Normal
230	30/1/2005	2:25:43.7	8.03	94.18	12.0	5.0	2	309	30	40	60	215	12	50	−130	245	54	−52	C9	Normal
231	30/1/2005	2:35:17.8	8.06	94.23	12.0	5.2	2	309	51	41	39	218	1	62	−151	256	65	−31	C9	Strike-slip
232	30/1/2005	3:13:38.1	8.06	94.25	19.1	5.1	7	124	83	292	1	33	168	84	176	259	86	6	C9	Strike-slip
233	30/1/2005	3:44:13.3	8.00	94.08	12.0	4.8	11	306	25	211	62	58	64	41	−49	195	61	−119	C9	Normal
234	30/1/2005	8:49:39.5	7.94	94.18	12.0	5.2	5	135	28	227	62	35	198	47	−130	68	56	−56	C9	Normal
235	30/1/2005	10:32:55.4	8.04	94.22	12.0	5.0	1	131	58	39	32	222	261	67	−23	1	69	−155	C9	Strike-slip
236	30/1/2005	15:33:16.4	8.14	94.22	12.0	5.5	2	116	39	24	51	209	239	55	−40	355	58	−137	C9	Strike-slip
237	30/1/2005	21:39:5.4	8.13	94.24	15.8	5.3	14	319	70	185	14	53	96	70	0	6	90	160	C9	Strike-slip
238	31/1/2005	2:20:43.8	8.02	94.23	18.5	4.8	4	152	25	60	64	250	267	47	−54	40	54	−122	C9	Normal
239	31/1/2005	8:15:7.2	8.09	94.22	12.0	5.1	5	311	66	51	24	219	357	70	−166	262	77	−21	C9	Strike-slip
240	31/1/2005	13:14:34.7	8.03	94.22	12.0	5.1	0	136	87	38	3	226	271	88	−2	1	88	−178	C9	Strike-slip
241	31/1/2005	16:30:20.4	8.09	94.26	12.0	5.1	4	117	37	24	53	212	239	52	−41	357	59	−134	C9	Normal
242	1/2/2005	1:8:3.4	7.81	94.21	12.0	5.3	13	100	58	212	29	3	145	60	−168	49	80	−31	C9	Strike-slip
243	1/2/2005	13:41:55.8	8.08	94.22	12.0	5.2	7	315	20	47	69	206	24	42	−120	242	55	−66	C9	Normal
244	2/2/2005	0:52:45.3	8.09	94.32	12.0	4.8	12	123	17	29	69	246	234	36	−60	18	59	−110	C9	Normal
245	2/2/2005	13:22:38.5	8.09	94.27	12.0	5.1	2	314	86	185	3	44	89	86	0	179	90	−176	C9	Strike-slip
246	4/2/2005	9:44:54.5	7.76	94.20	13.0	5.4	4	112	72	215	17	20	157	75	−171	65	81	−16	C9	Strike-slip
247	5/2/2005	8:0:30.5	8.06	94.26	12.0	5.4	8	122	7	31	79	260	221	37	−78	26	54	−99	C9	Normal
248	5/2/2005	17:35:47.1	8.08	94.27	15.0	5.9	6	317	84	131	1	227	2	85	176	92	86	5	C9	Strike-slip
249	6/2/2005	6:7:58.6	8.07	94.23	12.0	5.4	1	121	38	30	52	213	243	55	−42	360	57	−137	C9	Strike-slip
250	10/2/2005	1:34:32.1	8.01	94.20	12.0	5.0	8	125	31	220	58	23	184	46	−136	60	60	−53	C9	Normal
251	16/2/2005	8:19:45.6	8.17	94.23	13.0	5.9	6	306	84	123	0	216	351	85	176	82	86	5	C9	Strike-slip
252	24/2/2005	15:6:51.7	8.68	93.76	28.0	4.8	3	262	17	171	73	2	9	45	−65	157	50	−112	C9	Normal
253	25/2/2005	13:31:16.4	7.71	94.23	15.0	5.6	13	109	59	221	28	12	153	61	−169	58	80	−30	C9	Strike-slip
254	11/3/2005	12:59:54.9	7.47	94.38	12.8	5.1	16	98	58	215	27	359	141	59	−172	47	83	−31	C9	Strike-slip
255	26/4/2005	14:1:43.9	7.74	94.04	12.0	4.9	12	106	19	11	67	225	219	37	−57	360	59	−113	C9	Normal
256	27/4/2005	14:4:47.4	8.66	93.72	17.9	5.0	1	112	27	21	63	205	227	50	−53	358	52	−125	C9	Normal
257	13/6/2005	19:28:17.2	7.68	94.06	12.0	5.3	16	106	34	5	51	218	235	41	−32	350	69	−126	C9	Normal
258	27/6/2006	15:2:22	8.81	93.75	19.5	5.1	0	78	63	168	27	347	126	71	−160	29	71	−20	C9	Strike-slip
259	29/1/2007	19:48:40.8	8.37	93.76	77.3	5.5	30	98	57	251	12	1	136	60	167	233	78	31	C9	Strike-slip
260	31/5/2007	23:18:5.1	8.31	94.03	12.0	5.5	20	83	63	218	17	346	124	63	178	215	88	27	C9	Strike-slip
261	15/7/2005	12:50:7.7	7.56	94.30	13.9	4.9	16	112	39	215	47	4	161	45	−153	51	71	−48	C9	Normal
262	9/8/2005	11:23:2.7	7.78	94.33	24.0	5.4	15	104	73	256	7	12	147	74	175	239	85	16	C9	Strike-slip
263	18/9/2005	3:47:41.8	7.60	94.16	12.0	5.1	25	103	2	194	65	289	189	20	−96	15	70	−88	C9	Normal
264	6/10/2005	2:53:0.9	7.74	93.98	18.6	4.9	16	107	25	10	60	228	229	36	−45	358	66	−117	C9	Normal
265	21/11/2007	19:4:2.1	7.76	93.79	17.8	4.9	5	341	10	71	79	226	60	41	−105	260	50	−77	C9	Normal
266	21/11/2007	19:4:2.1	7.76	93.79	17.8	4.9	5	341	10	71	79	226	60	41	−105	260	50	−77	C9	Normal
267	13/2/1982	19:56:16.9	5.81	94.68	66.2	5.7	21	52	68	219	4	320	94	72	168	188	78	19	C10	Strike-slip
268	30/1/1983	1:26:3	5.36	94.84	75.4	5.2	19	47	23	308	59	173	169	32	−44	298	68	−115	C10	Normal
269	4/4/1983	2:51:43.7	5.72	94.65	71.6	7.0	61	51	29	234	1	143	207	51	51	78	53	127	C10	Thrust
270	2/7/1983	9:34:8.4	5.81	94.75	87.1	5.8	61	69	28	230	8	325	83	44	132	211	59	57	C10	Thrust
271	17/9/1983	5:56:59.5	4.60	95.10	45.2	6.1	17	49	40	304	45	157	182	45	−25	289	73	−132	C10	Normal
272	27/12/1988	13:50:43.6	4.65	95.21	111.4	5.3	24	10	30	114	50	247	56	34	−152	303	75	−59	C10	Normal
273	4/1/2005	19:8:6.5	5.17	94.29	34.4	5.2	64	81	6	340	26	247	323	20	73	162	71	96	C10	Thrust
274	5/1/2005	14:34:35.4	5.20	94.63	52.9	5.3	75	21	7	138	13	230	329	33	103	134	58	82	C10	Thrust
275	5/1/2005	14:54:6.2	5.32	94.24	33.0	5.9	66	47	2	142	24	232	326	21	95	141	69	88	C10	Thrust
276	6/1/2005	0:56:31.2	5.02	94.60	54.0	5.7	73	27	6	136	16	228	327	29	102	133	62	83	C10	Thrust
277	16/3/2006	15:12:16.8	4.84	94.64	46.5	5.0	72	18	7	131	16	223	324	29	105	127	62	82	C10	Thrust
278	17/8/2000	18:40:12.6	5.77	94.63	65.8	5.7	12	52	68	174	18	319	96	69	−175	5	86	−21	C10	Strike-slip
279	31/10/2001	22:4:39.2	5.21	94.20	34.4	5.7	9	266	23	0	65	156	331	41	−126	195	58	−63	C10	Normal
280	27/12/2004	0:32:20.2	5.36	94.33	39.0	5.8	69	55	1	321	21	230	318	24	87	142	66	92	C10	Thrust
281	11/1/2005	21:46:36.4	4.74	94.63	48.0	5.0	75	37	2	133	15	223	316	30	93	132	60	88	C10	Thrust
282	12/1/2005	13:58:22.7	5.33	94.51	43.0	5.4	72	34	4	137	17	228	324	28	99	135	62	85	C10	Thrust
283	12/1/2005	18:44:47.4	5.16	94.41	47.2	5.1	70	53	3	151	20	242	338	25	97	150	65	87	C10	Thrust
284	4/5/2005	5:58:54	4.60	94.87	42.0	5.3	16	46	60	166	25	308	89	60	−174	355	84	−30	C10	Strike-slip
285	5/5/2005	1:14:52.6	5.18	94.18	38.4	5.0	75	63	1	156	15	246	337	30	91	155	60	89	C10	Thrust
286	9/5/2005	1:30:56	4.85	94.76	40.0	5.2	71	39	2	135	19	226	319	26	95	134	64	88	C10	Thrust
287	12/5/2005	16:4:29	5.01	94.47	19.0	5.2	54	77	0	168	36	258	349	9	91	168	81	90	C10	Thrust
288	21/5/2005	23:1:17.2	5.03	94.71	44.0	5.6	68	37	4	137	21	228	325	24	100	135	66	86	C10	Thrust
289	31/5/2005	2:29:36.3	5.23	94.57	20.5	5.5	49	105	7	7	40	272	311	8	33	188	86	97	C10	Thrust
290	31/5/2005	7:28:5.9	5.21	94.60	52.4	5.0	75	31	7	149	13	240	340	32	103	144	59	82	C10	Thrust
291	27/12/2004	8:21:41.5	5.20	94.48	55.1	5.3	76	47	1	315	14	225	314	31	89	135	59	91	C10	Thrust
292	27/12/2004	9:39:10.6	5.21	94.48	41.0	6.0	66	38	3	134	24	225	320	21	97	133	69	87	C10	Thrust
293	28/12/2004	14:30:44.7	4.49	95.06	46.3	5.0	17	47	72	248	6	139	184	74	8	92	82	163	C10	Strike-slip
294	29/12/2004	7:52:56.6	5.01	94.82	17.5	5.3	46	40	8	138	43	236	35	8	167	138	88	82	C10	Thrust
295	29/12/2004	15:50:9	5.36	94.53	48.5	5.1	74	35	5	142	15	233	330	30	99	139	61	85	C10	Thrust
296	29/12/2004	18:50:23	5.33	94.13	43.4	5.4	72	35	4	136	17	228	323	28	98	135	62	86	C10	Thrust
297	29/12/2004	21:13:3.1	5.13	94.61	41.0	5.6	28	35	32	144	45	273	76	34	−162	331	80	−58	C10	Normal
298	30/12/2004	4:27:39	5.34	94.29	36.3	5.2	69	31	6	137	20	229	330	26	104	135	65	83	C10	Thrust
299	30/12/2004	21:36:5.1	5.12	94.28	42.0	5.4	72	34	5	140	17	232	330	28	101	138	62	84	C10	Thrust
300	30/12/2004	23:4:58.8	5.24	94.30	43.8	4.9	74	333	15	126	7	218	324	40	113	115	54	72	C10	Thrust
301	31/12/2004	10:58:28.6	4.85	94.57	49.2	5.2	75	29	4	136	14	227	324	31	99	134	60	85	C10	Thrust
302	31/12/2004	14:38:47.6	4.79	94.66	49.6	5.4	73	36	2	132	17	223	316	28	94	131	62	88	C10	Thrust
303	31/12/2004	17:48:8.2	4.68	95.09	24.0	5.9	48	46	0	137	42	227	326	3	100	137	87	90	C10	Thrust
304	1/1/2005	4:3:14	5.36	94.29	35.0	5.7	65	26	9	135	23	228	335	23	112	131	69	81	C10	Thrust
305	2/1/2005	12:12:17.7	5.41	94.31	34.0	5.3	61	28	11	139	26	234	349	21	122	135	72	78	C10	Thrust
306	2/1/2005	19:35:26.3	5.22	94.15	71.8	5.1	57	37	14	150	29	248	11	21	133	146	75	75	C10	Thrust
307	8/1/2005	5:58:24.2	4.69	94.76	21.8	5.1	49	77	7	175	40	271	55	9	150	175	86	83	C10	Thrust
308	9/1/2005	22:13:0.3	4.63	94.94	46.0	6.0	67	45	1	313	23	223	311	22	88	133	68	91	C10	Thrust
309	22/1/2005	12:58:36.5	4.94	94.74	40.0	4.9	39	57	50	226	5	323	92	59	154	197	68	34	C10	Strike-slip
310	25/1/2005	9:54:26.5	5.15	94.60	58.6	5.0	76	39	1	133	14	223	314	31	92	132	59	89	C10	Thrust
311	26/1/2005	23:43:29.8	5.07	94.36	51.9	5.1	71	70	1	162	19	253	344	26	92	162	64	89	C10	Thrust
312	27/1/2005	20:9:56.1	5.41	94.24	31.0	5.5	64	38	4	137	25	229	329	20	103	136	70	85	C10	Thrust
313	29/1/2005	2:55:22.8	4.84	94.52	52.0	5.1	73	66	6	318	16	226	308	29	78	141	62	96	C10	Thrust
314	29/1/2005	18:21:1.8	5.25	94.15	46.0	5.2	76	41	1	135	14	225	316	31	92	134	59	89	C10	Thrust
315	2/2/2005	9:4:29.2	5.17	94.41	32.0	5.2	65	38	5	140	24	232	334	21	105	138	69	84	C10	Thrust
316	9/2/2005	13:27:28.9	4.51	95.03	47.0	6.0	70	43	1	312	20	222	310	25	89	132	65	91	C10	Thrust
317	13/2/2005	1:22:11.4	4.82	94.61	51.0	5.4	73	25	5	133	16	225	323	30	101	130	61	84	C10	Thrust
318	13/2/2005	2:2:8.6	4.85	94.70	42.0	5.2	71	30	5	134	18	225	323	27	100	132	63	85	C10	Thrust
319	18/2/2005	19:33:48	5.31	94.35	36.0	5.6	66	33	5	135	23	227	327	22	103	133	68	85	C10	Thrust
320	19/2/2005	23:45:16	4.97	94.37	33.9	4.8	81	349	9	155	2	246	345	44	103	147	48	78	C10	Thrust
321	12/3/2005	22:33:14.9	5.16	94.62	54.6	5.2	76	54	3	313	14	223	309	31	85	135	59	93	C10	Thrust
322	13/3/2005	22:12:48.3	5.42	94.42	42.0	5.4	70	25	8	138	18	231	334	28	107	134	63	81	C10	Thrust
323	16/3/2005	6:39:52.7	5.37	94.32	35.0	5.4	61	20	13	135	25	231	349	23	126	131	72	76	C10	Thrust
324	17/3/2005	23:20:51.2	4.66	94.93	45.0	5.8	68	42	0	133	22	223	313	23	90	133	67	90	C10	Thrust
325	25/3/2005	1:4:55.2	5.30	94.25	34.0	5.9	66	45	3	141	24	232	328	22	97	140	69	87	C10	Thrust
326	30/3/2005	23:17:15.5	5.46	94.19	38.9	5.0	83	77	0	168	7	258	348	38	90	168	52	90	C10	Thrust
327	31/3/2005	14:27:32.9	5.09	94.54	36.2	4.8	77	97	6	342	12	251	333	33	79	166	57	97	C10	Thrust
328	4/4/2005	19:37:10.4	4.75	94.73	42.8	4.8	1	338	17	68	73	245	51	47	−114	264	48	−67	C10	Normal
329	17/6/2005	2:37:41	5.33	94.64	46.0	5.3	70	19	10	139	17	232	337	30	111	133	62	79	C10	Thrust
330	13/8/2006	8:41:51.3	5.27	94.54	54.3	5.2	75	27	4	133	15	224	320	31	99	130	60	85	C10	Thrust
331	16/9/2006	6:17:47.2	4.84	94.59	49.3	5.3	70	8	11	130	16	224	330	30	112	125	62	78	C10	Thrust
332	12/10/2006	5:30:40	4.80	95.09	41.0	5.0	84	135	6	312	0	42	138	45	98	306	46	82	C10	Thrust
333	9/12/2006	9:24:50.4	4.80	94.59	53.3	5.1	76	36	2	135	13	226	319	32	94	134	58	87	C10	Thrust
334	17/12/2006	21:10:26	4.58	94.89	54.4	5.8	72	38	1	131	18	222	314	27	93	131	63	89	C10	Thrust
335	3/1/2007	12:47:33.7	5.25	94.28	44.0	5.4	71	25	7	136	18	228	329	28	105	132	63	82	C10	Thrust
336	27/4/2007	8:2:52.2	5.09	94.43	49.2	5.9	70	38	2	134	20	225	319	25	95	133	65	88	C10	Thrust
337	1/5/2007	19:44:20.9	5.29	94.38	51.2	5.0	73	9	11	137	13	230	334	33	110	131	59	77	C10	Thrust
338	24/6/2007	13:47:40.3	5.21	94.50	54.0	5.0	77	37	1	134	13	224	316	32	93	133	58	88	C10	Thrust
339	23/7/2005	0:45:1.4	5.45	94.37	32.0	5.0	64	71	1	339	26	249	336	19	87	160	71	91	C10	Thrust
340	23/7/2005	22:53:38.5	5.03	94.47	46.9	5.3	71	19	10	141	16	234	338	31	110	135	62	78	C10	Thrust
341	30/7/2005	15:13:23.4	5.16	94.32	31.0	5.8	56	26	12	135	31	232	356	18	133	132	77	77	C10	Thrust
342	2/8/2005	20:56:40.6	5.22	94.25	34.5	5.0	78	32	4	140	11	231	326	34	97	138	56	86	C10	Thrust
343	26/8/2005	0:36:56.5	5.13	94.58	62.2	4.8	78	62	4	313	11	222	307	34	83	136	56	95	C10	Thrust
344	28/8/2005	4:43:42.3	5.30	94.57	43.0	5.3	71	26	6	132	19	224	323	27	102	130	64	84	C10	Thrust
345	1/9/2005	16:42:42.7	4.77	94.63	51.0	5.1	73	14	8	134	14	226	328	32	106	129	60	80	C10	Thrust
346	7/9/2005	6:42:54.1	5.05	94.66	60.4	5.0	71	84	13	313	14	220	293	33	66	141	60	105	C10	Thrust
347	10/9/2005	16:57:51.3	4.61	94.98	46.0	5.8	68	37	1	130	22	220	313	23	93	129	67	89	C10	Thrust
348	3/10/2005	22:9:27.3	5.31	94.35	34.0	5.5	64	23	8	129	25	223	330	21	112	126	71	82	C10	Thrust
349	4/10/2005	12:23:26.9	5.37	94.14	41.1	5.0	72	34	5	139	17	231	328	28	100	137	62	85	C10	Thrust
350	11/10/2005	15:5:44	4.49	95.02	49.0	5.9	70	42	0	311	20	221	311	25	89	131	65	90	C10	Thrust
351	13/1/2006	14:47:33.5	4.86	94.49	40.5	4.8	71	26	7	137	18	229	330	28	105	133	63	82	C10	Thrust
352	15/2/2006	1:17:56	5.26	94.18	46.7	4.8	70	349	15	125	14	218	328	34	117	116	60	73	C10	Thrust
353	26/2/2006	21:32:53.4	5.27	94.59	53.8	5.2	73	19	8	136	15	228	328	31	105	131	60	81	C10	Thrust
354	13/5/2006	3:11:44.2	5.33	94.30	43.1	5.7	72	47	1	139	18	229	320	28	91	139	63	89	C10	Thrust
355	14/6/2006	0:14:33.7	5.27	94.41	52.3	5.2	71	12	11	139	15	232	338	32	112	132	61	77	C10	Thrust
356	5/1/2008	20:1:56.9	5.21	94.62	56.7	5.3	74	13	8	130	14	222	323	32	104	126	59	81	C10	Thrust
357	5/3/2008	17:4:6	4.68	94.71	49.8	5.0	75	23	5	130	14	221	318	31	99	127	60	85	C10	Thrust
358	8/5/2008	11:31:26.6	5.21	94.49	52.8	5.0	73	358	10	123	14	215	318	32	108	117	59	79	C10	Thrust
359	23/7/1991	13:25:48.4	3.90	95.83	42.3	5.6	36	359	10	261	52	158	132	13	−38	260	82	−100	C11	Normal
360	19/3/2006	4:24:35.8	3.84	95.96	56.6	5.2	54	116	27	340	21	239	291	34	35	170	71	118	C11	Thrust
361	21/7/2005	1:42:44.7	4.07	96.12	18.6	5.2	9	304	71	62	16	211	348	72	−175	257	85	−18	C11	Strike-slip
362	22/9/2005	12:30:9.1	3.74	95.89	46.0	5.1	56	325	24	95	23	196	324	30	143	87	72	65	C11	Thrust
363	25/4/2005	3:18:35.5	3.08	93.87	20.8	4.9	73	110	11	340	12	247	323	34	70	166	58	103	C12	Thrust
364	14/1/2005	21:38:20	3.01	93.81	12.0	5.6	81	126	9	315	1	225	306	44	77	143	47	102	C12	Thrust
365	24/5/2005	9:37:55.2	2.48	94.41	12.0	5.2	76	4	7	124	12	215	315	33	103	119	58	81	C12	Thrust
366	27/12/2004	18:9:32.1	2.61	94.42	12.0	5.3	68	74	7	326	20	234	311	25	74	149	66	98	C12	Thrust
367	28/12/2004	14:48:30.1	3.24	93.68	12.0	4.9	82	284	6	150	6	59	142	39	81	334	51	98	C12	Thrust
368	29/12/2004	14:3:24.3	3.19	93.80	12.8	5.1	76	229	3	331	14	62	156	31	96	330	59	86	C12	Thrust
369	23/1/2005	20:36:8.9	2.66	94.31	16.6	5.2	22	310	62	169	16	47	90	63	5	358	86	153	C12	Strike-slip
370	29/1/2005	6:10:44	3.21	93.59	12.0	5.5	86	132	4	329	1	239	325	44	85	152	46	95	C12	Thrust
371	29/1/2005	7:21:45.2	3.04	93.74	12.0	5.2	62	320	27	157	7	63	125	45	49	356	58	123	C12	Thrust
372	1/2/2005	17:14:3.2	2.67	94.21	12.0	4.8	78	223	1	130	12	40	129	33	89	311	57	91	C12	Thrust
373	21/2/2005	6:10:11.7	3.25	93.67	12.0	5.2	77	179	11	325	7	57	159	39	108	317	53	76	C12	Thrust
374	27/7/2005	14:5:29	3.28	93.73	18.7	4.7	74	190	11	321	12	53	157	34	109	314	58	77	C12	Thrust
375	2/12/2005	3:8:1.4	3.18	93.82	18.6	4.8	79	165	10	318	5	49	150	41	105	310	51	77	C12	Thrust
376	22/3/1982	8:38:36.1	1.92	96.85	15.0	5.6	59	73	14	318	27	221	281	22	51	143	73	104	C13	Thrust
377	20/12/1988	3:35:16.9	1.87	97.16	15.0	5.5	47	27	3	120	43	212	349	4	139	119	88	87	C13	Thrust
378	2/8/1989	10:24:29	2.66	95.92	50.8	5.4	63	7	16	132	21	229	345	28	126	125	67	72	C13	Thrust
379	15/4/2005	13:8:56	2.88	96.34	12.0	5.3	74	279	0	10	16	100	191	29	91	10	61	89	C13	Thrust
380	17/4/2005	13:43:55.2	0.31	97.75	12.0	5.4	37	68	3	336	52	241	178	8	−67	335	82	−93	C13	Normal
381	18/4/2005	13:25:38.2	0.87	97.12	30.1	5.0	66	43	3	141	24	232	330	22	99	139	69	86	C13	Thrust
382	24/4/2005	10:59:7	2.09	96.22	36.0	4.7	67	358	12	118	19	212	321	28	115	112	65	77	C13	Thrust
383	25/4/2005	13:58:35.3	2.27	96.80	31.3	4.8	60	91	22	317	19	219	277	32	45	146	68	114	C13	Thrust
384	12/3/2006	19:44:54	1.30	97.13	32.0	4.8	65	352	16	118	19	214	328	29	124	111	66	73	C13	Thrust
385	1/9/1993	14:3:23.5	2.85	95.92	15.0	6.3	54	43	1	311	36	221	306	9	85	132	81	91	C13	Thrust
386	31/10/1994	11:48:18.3	2.63	96.00	37.2	6.2	64	59	12	304	23	209	276	24	59	129	69	103	C13	Thrust
387	14/3/1995	10:27:34.1	2.78	95.63	29.4	5.5	71	53	5	308	18	217	299	27	79	131	64	95	C13	Thrust
388	3/6/1995	11:57:36.9	2.91	95.62	48.9	5.1	70	5	10	122	18	215	320	29	110	117	63	79	C13	Thrust
389	22/11/1995	13:27:58.2	2.85	95.72	34.8	5.8	65	65	11	310	22	216	285	25	63	135	68	102	C13	Thrust
390	13/9/1996	5:4:40.8	3.04	95.52	34.6	5.3	71	19	7	131	17	223	324	29	105	127	62	82	C13	Thrust
391	7/7/1997	11:24:41.8	0.86	97.16	32.2	5.9	59	55	6	316	31	222	294	15	68	137	76	96	C13	Thrust
392	24/2/1999	7:20:48.3	3.08	96.32	24.5	5.4	49	41	10	300	39	202	237	11	27	121	85	100	C13	Thrust
393	7/3/2001	8:29:26.7	0.34	97.68	36.2	5.1	57	69	15	315	29	217	272	21	45	139	75	105	C13	Thrust
394	2/11/2002	1:26:25.9	2.65	95.99	23.0	7.3	60	52	5	314	30	221	297	16	73	135	75	95	C13	Thrust
395	2/11/2002	9:46:53.4	2.89	96.05	27.0	6.3	55	77	7	336	34	241	303	13	56	158	79	98	C13	Thrust
396	13/11/2002	15:53:12.6	2.86	95.74	31.0	5.6	63	41	3	306	27	214	297	18	81	127	72	93	C13	Thrust
397	30/11/2002	4:7:9.9	2.51	96.11	41.1	5.2	30	97	47	328	27	204	242	47	2	150	88	137	C13	Strike-slip
398	28/6/2003	7:36:45.8	2.77	95.76	20.0	5.2	39	84	29	327	38	213	239	29	1	148	89	119	C13	Thrust
399	15/9/2003	12:14:34.8	2.16	96.12	38.9	5.1	54	80	31	293	16	193	247	40	36	128	68	124	C13	Thrust
400	11/5/2004	8:28:51.3	0.18	97.58	24.0	6.1	59	35	3	130	31	222	322	14	102	130	76	87	C13	Thrust
401	17/7/2004	13:38:4.8	1.07	97.36	38.2	5.1	55	101	31	311	14	212	267	41	38	146	66	125	C13	Thrust
402	4/5/2005	0:42:2.6	0.23	96.89	15.2	5.2	6	65	62	167	27	332	112	67	−164	16	76	−24	C13	Strike-slip
403	4/5/2005	0:44:50.1	2.80	96.17	50.6	5.1	0	292	68	22	22	202	339	74	−164	245	75	−16	C13	Strike-slip
404	10/5/2005	22:22:47.6	0.90	97.10	20.0	5.1	60	40	1	131	30	222	314	15	92	131	75	89	C13	Thrust
405	10/5/2005	22:29:44.9	0.93	97.00	22.0	5.3	64	52	2	318	26	227	312	19	84	139	71	92	C13	Thrust
406	16/5/2005	9:58:51.7	0.63	97.73	21.6	5.1	66	100	3	4	24	273	357	21	83	185	69	93	C13	Thrust
407	19/5/2005	1:55:2.5	1.88	96.74	12.0	6.9	52	49	3	315	38	222	290	8	65	135	83	93	C13	Thrust
408	19/5/2005	20:44:7.9	0.49	97.26	19.4	5.0	26	35	9	301	63	193	144	21	−65	298	71	−99	C13	Normal
409	21/5/2005	9:43:52.2	1.09	97.18	36.0	5.1	49	325	37	116	14	217	346	45	149	99	69	50	C13	Thrust
410	23/5/2005	5:48:23.8	0.70	97.26	33.0	4.9	75	32	4	137	15	228	323	31	98	134	60	85	C13	Thrust
411	24/5/2005	11:38:43.9	1.21	97.23	31.6	4.8	39	108	46	320	17	211	257	50	19	155	76	138	C13	Strike-slip
412	25/5/2005	18:47:45.5	1.32	97.24	33.4	4.9	75	59	5	311	14	219	303	31	81	133	59	96	C13	Thrust
413	3/6/2005	0:42:4.7	1.21	96.96	12.0	5.8	55	41	4	137	35	230	338	11	112	136	80	86	C13	Thrust
414	27/12/2004	6:59:15.2	2.95	95.42	13.1	5.6	40	42	5	307	50	211	174	7	−43	307	85	−95	C13	Normal
415	27/12/2004	20:10:52.4	2.92	95.49	12.0	5.8	79	148	11	324	1	54	155	45	106	313	47	75	C13	Thrust
416	1/1/2005	23:40:32.6	2.74	96.33	57.7	4.9	69	87	15	313	14	219	289	33	62	141	61	107	C13	Thrust
417	15/1/2005	16:44:7.1	2.68	95.98	34.5	4.9	31	324	59	137	3	232	4	67	159	102	71	25	C13	Strike-slip
418	21/1/2005	8:37:4.7	1.37	97.42	31.3	4.8	75	342	11	120	10	212	316	36	110	112	56	76	C13	Thrust
419	26/1/2005	16:50:6.8	2.69	96.21	60.1	4.8	42	94	43	308	18	201	246	47	20	142	75	135	C13	Thrust
420	26/2/2005	12:56:58.1	2.80	95.40	12.0	6.7	51	51	3	318	39	226	294	6	66	139	84	93	C13	Thrust
421	3/3/2005	17:10:23.5	2.77	95.49	40.4	4.8	16	188	3	97	73	358	282	29	−84	95	61	−93	C13	Normal
422	28/3/2005	16:10:31.5	1.67	97.07	25.8	8.7	52	30	4	125	38	218	333	8	118	125	83	86	C13	Thrust
423	29/3/2005	4:50:8.6	0.30	96.95	28.3	5.5	3	52	21	321	69	150	163	46	−60	304	51	−117	C13	Normal
424	29/3/2005	5:16:31	2.39	96.39	30.0	5.9	62	19	3	114	28	205	302	17	99	113	73	87	C13	Thrust
425	29/3/2005	9:42:57.9	0.49	97.10	35.3	5.2	76	43	3	300	14	210	296	32	84	122	59	93	C13	Thrust
426	29/3/2005	14:16:8.6	2.62	95.99	23.0	5.1	18	47	22	310	61	173	167	33	−48	300	66	−114	C13	Normal
427	29/3/2005	18:29:47.5	1.01	97.73	18.0	5.0	16	350	0	260	74	170	80	29	−90	260	61	−90	C13	Normal
428	29/3/2005	20:41:39.3	1.86	97.02	58.5	5.2	72	84	15	300	10	207	279	37	65	130	57	108	C13	Thrust
429	30/3/2005	0:25:52.9	0.78	97.16	33.0	5.0	72	347	13	121	13	213	320	34	113	113	59	75	C13	Thrust
430	30/3/2005	23:12:6	1.03	97.08	30.6	5.0	65	358	16	124	19	220	334	29	123	117	66	73	C13	Thrust
431	30/3/2005	23:19:16.1	1.14	96.91	36.8	4.9	83	353	7	161	2	252	349	44	101	154	47	80	C13	Thrust
432	30/3/2005	23:40:49.2	1.50	96.84	24.0	5.2	58	63	13	311	28	213	271	21	49	135	75	104	C13	Thrust
433	31/3/2005	8:30:28.8	2.65	96.14	24.0	5.0	15	73	25	336	60	192	194	37	−45	323	65	−118	C13	Normal
434	31/3/2005	16:30:1.8	1.21	96.94	30.0	5.0	73	34	4	138	16	229	325	29	99	135	61	85	C13	Thrust
435	31/3/2005	18:2:35.2	0.29	97.57	17.5	4.9	69	1	8	114	19	207	311	27	109	110	65	81	C13	Thrust
436	1/4/2005	0:49:42	0.51	97.15	16.7	5.0	23	117	62	332	14	213	256	63	7	163	84	153	C13	Strike-slip
437	1/4/2005	7:40:29.1	2.35	96.18	12.0	4.9	55	39	4	135	35	228	337	11	112	134	80	86	C13	Thrust
438	1/4/2005	10:37:46.1	2.80	96.34	12.0	5.2	8	314	4	45	81	161	39	37	−97	228	53	−85	C13	Normal
439	1/4/2005	14:18:17.6	2.20	96.65	36.3	4.8	75	63	6	311	14	219	301	31	79	134	59	97	C13	Thrust
440	1/4/2005	17:24:50	1.16	97.23	21.0	5.1	66	62	8	315	23	221	297	23	70	138	68	98	C13	Thrust
441	2/4/2005	3:37:22	0.75	97.17	12.0	5.0	2	289	75	26	15	199	335	78	−171	243	81	−12	C13	Strike-slip
442	2/4/2005	16:24:14.7	2.68	96.35	19.0	5.0	9	133	12	225	75	9	209	38	−110	54	55	−75	C13	Normal
443	3/4/2005	12:21:20.5	2.89	96.32	17.8	5.1	80	290	1	28	10	118	210	35	92	27	55	88	C13	Thrust
444	3/4/2005	20:23:36.3	1.98	96.72	35.3	4.8	72	38	0	306	18	216	305	27	89	127	63	91	C13	Thrust
445	3/4/2005	22:31:56.9	1.00	97.17	33.2	4.8	74	42	10	172	12	264	7	34	108	165	58	78	C13	Thrust
446	4/4/2005	11:5:45.2	1.18	97.17	30.5	4.9	68	341	19	131	10	225	337	39	122	119	58	67	C13	Thrust
447	5/4/2005	9:37:30	1.58	97.00	43.4	5.2	0	298	77	29	13	208	344	81	−171	253	81	−10	C13	Strike-slip
448	6/4/2005	10:11:39	2.37	96.15	27.5	4.9	82	67	3	183	7	273	7	38	96	180	52	86	C13	Thrust
449	7/4/2005	2:21:30.4	1.09	96.98	23.0	5.0	67	17	11	134	20	229	338	27	116	129	66	78	C13	Thrust
450	7/4/2005	11:46:2.8	0.52	97.31	12.0	5.6	41	97	49	276	0	7	134	62	149	239	63	31	C13	Strike-slip
451	7/4/2005	11:50:26.2	0.88	97.40	34.8	5.2	72	146	12	276	13	9	114	33	111	269	59	77	C13	Thrust
452	7/4/2005	15:24:5.4	1.30	96.88	26.0	5.1	63	70	6	328	26	235	312	20	73	150	71	96	C13	Thrust
453	8/4/2005	1:51:38.4	0.50	97.34	12.0	5.7	5	282	82	51	6	191	326	82	−179	236	89	−8	C13	Strike-slip
454	9/4/2005	19:3:36.7	1.14	96.94	29.0	4.9	72	11	14	153	11	246	353	37	115	143	57	73	C13	Thrust
455	25/4/2005	20:18:30.6	0.48	97.11	12.0	5.3	17	34	20	298	63	161	152	33	−51	288	65	−112	C13	Normal
456	25/4/2005	20:22:18	0.47	97.45	31.3	4.8	14	25	38	283	48	131	154	45	−30	266	69	−131	C13	Normal
457	25/4/2005	21:40:16.4	0.43	97.28	13.2	5.2	25	50	0	140	65	230	140	20	−90	320	70	−90	C13	Normal
458	26/4/2005	17:18:26.3	1.14	97.01	19.0	5.3	57	37	4	132	32	224	327	13	106	131	77	86	C13	Thrust
459	2/5/2005	12:3:21.2	1.18	96.95	29.1	4.8	66	75	10	322	22	228	300	25	66	146	67	101	C13	Thrust
460	11/6/2005	3:47:47	0.80	97.29	26.0	5.2	61	36	3	131	29	223	321	17	100	130	74	87	C13	Thrust
461	21/6/2006	8:53:35.7	0.95	97.01	34.3	4.9	70	68	9	311	18	218	293	29	70	136	63	101	C13	Thrust
462	27/7/2006	11:16:44.5	1.66	97.01	15.0	6.3	50	38	2	131	40	223	336	5	115	131	85	88	C13	Thrust
463	3/9/2006	16:20:34.9	0.10	97.11	30.5	5.5	21	50	1	140	69	234	137	24	−93	321	66	−89	C13	Normal
464	4/10/2006	13:33:49.1	1.15	97.61	37.3	5.0	69	336	17	121	11	214	325	37	120	110	59	70	C13	Thrust
465	6/10/2006	14:49:4.2	0.76	97.22	34.5	5.3	56	332	28	113	18	213	339	36	142	101	69	60	C13	Thrust
466	25/10/2006	5:6:6.7	0.93	97.12	30.8	5.2	68	36	5	138	22	229	328	24	102	135	67	85	C13	Thrust
467	25/10/2006	5:19:48.6	0.78	97.26	35.7	5.0	74	34	1	129	16	219	311	29	93	128	61	88	C13	Thrust
468	9/11/2006	15:55:48.9	1.03	97.19	18.2	5.2	26	355	7	88	63	192	70	20	−109	271	71	−83	C13	Normal
469	25/1/2007	15:18:40.1	1.36	97.03	39.6	5.1	62	331	23	115	15	212	331	37	132	103	64	64	C13	Thrust
470	14/2/2007	19:50:2.1	0.33	97.22	12.0	5.7	70	328	17	116	10	209	320	38	119	105	57	69	C13	Thrust
471	14/2/2007	20:46:34.2	0.39	97.17	12.0	5.5	69	327	14	98	15	191	300	32	116	90	61	74	C13	Thrust
472	18/2/2007	10:45:29.1	0.98	97.26	30.9	5.1	70	44	2	139	20	230	323	25	94	138	65	88	C13	Thrust
473	1/3/2007	2:1:5.8	3.60	96.23	43.4	5.3	52	55	33	203	16	303	71	41	146	188	69	54	C13	Thrust
474	7/4/2007	9:51:54.4	2.74	95.48	12.0	6.1	52	51	3	317	38	225	293	8	65	138	83	93	C13	Thrust
475	8/9/2007	11:31:48.4	0.10	97.62	35.9	5.1	71	24	3	123	18	214	309	27	97	121	64	87	C13	Thrust
476	29/9/2007	5:37:8.8	2.71	95.39	15.0	6.0	52	56	4	321	38	227	288	8	57	141	83	94	C13	Thrust
477	18/6/2005	12:36:18.9	1.41	97.44	35.5	4.8	28	308	61	133	2	39	87	69	19	350	72	157	C13	Strike-slip
478	19/6/2005	12:45:2	1.09	97.09	21.0	5.0	69	45	1	139	21	229	322	24	93	138	66	89	C13	Thrust
479	27/6/2005	17:14:32.1	1.25	97.20	22.0	4.8	66	354	17	129	16	224	338	33	123	120	63	71	C13	Thrust
480	2/7/2005	9:10:37.9	1.09	96.95	12.0	5.0	55	59	1	328	35	238	325	10	87	148	80	91	C13	Thrust
481	5/7/2005	1:52:6.3	1.56	96.93	16.0	6.7	52	39	2	132	38	223	329	8	107	131	83	88	C13	Thrust
482	8/7/2005	21:28:20	0.88	97.29	12.0	4.7	28	300	56	84	17	201	337	57	171	72	82	33	C13	Strike-slip
483	11/7/2005	14:36:10.8	0.93	97.00	22.0	5.6	61	43	1	135	29	226	319	16	94	135	74	89	C13	Thrust
484	22/7/2005	9:50:7.2	2.27	96.97	15.0	5.2	44	36	2	304	46	211	189	3	−25	304	89	−92	C13	Normal
485	26/7/2005	1:39:3.7	1.75	97.08	41.2	5.0	44	310	44	109	11	209	339	51	153	87	69	42	C13	Strike-slip
486	27/7/2005	13:57:19.4	2.52	96.04	33.6	4.8	74	32	0	123	16	213	303	29	91	122	61	90	C13	Thrust
487	30/7/2005	0:36:31.9	0.91	97.13	26.0	5.3	55	41	6	139	34	233	346	12	118	138	79	84	C13	Thrust
488	30/7/2005	21:17:16.1	0.26	97.39	22.2	4.8	6	225	32	131	57	324	345	48	−45	109	58	−129	C13	Normal
489	31/7/2005	12:37:29.5	0.39	97.67	37.6	5.0	70	354	13	124	15	218	327	32	116	117	61	75	C13	Thrust
490	1/8/2005	13:17:53.4	1.41	97.35	32.4	4.7	49	330	39	126	12	226	354	47	148	106	67	48	C13	Thrust
491	13/8/2005	18:27:27.6	1.20	96.95	22.0	5.1	64	43	2	137	25	227	321	20	95	136	70	88	C13	Thrust
492	26/8/2005	6:7:1.7	1.93	96.80	32.0	4.8	80	23	6	150	8	240	337	38	99	145	53	83	C13	Thrust
493	28/8/2005	5:34:47.2	1.40	97.08	23.0	5.0	70	41	2	135	20	226	319	25	94	135	65	88	C13	Thrust
494	16/9/2005	17:19:35.5	2.47	96.17	31.4	4.8	69	80	13	313	16	219	290	31	64	140	63	105	C13	Thrust
495	19/9/2005	14:35:5.9	1.40	97.31	33.3	4.9	56	320	33	124	7	219	341	47	138	102	60	51	C13	Thrust
496	4/11/2005	17:44:49.9	0.97	96.96	21.0	5.5	61	42	2	136	28	226	321	17	96	135	74	88	C13	Thrust
497	22/11/2005	14:4:36.8	0.46	97.19	29.4	5.0	58	236	22	106	22	6	61	30	41	294	71	113	C13	Thrust
498	27/11/2005	23:31:40	0.92	96.98	22.0	5.6	62	37	5	136	28	229	332	18	106	135	73	85	C13	Thrust
499	3/12/2005	18:48:11.2	1.10	97.08	25.8	4.9	50	119	29	347	24	242	288	33	27	175	75	120	C13	Thrust
500	4/12/2005	14:9:32.7	0.65	97.43	39.0	4.9	9	126	71	9	16	219	261	72	−6	353	85	−162	C13	Strike-slip
501	6/12/2005	5:40:20.7	2.32	96.48	34.4	4.8	64	323	24	118	10	212	328	41	128	103	59	62	C13	Thrust
502	7/12/2005	2:19:31.3	1.11	96.90	32.5	5.2	68	46	0	316	22	226	315	23	90	136	67	90	C13	Thrust
503	7/12/2005	8:38:22.5	0.20	97.27	14.5	4.8	68	309	17	169	14	75	143	35	59	359	61	110	C13	Thrust
504	13/1/2006	10:50:5.5	1.22	97.58	31.2	5.1	71	358	13	131	14	224	332	34	115	123	60	74	C13	Thrust
505	13/1/2006	22:47:35.8	1.35	97.28	34.6	4.9	33	118	54	326	14	217	263	57	15	164	77	146	C13	Strike-slip
506	31/1/2006	19:15:53.9	2.34	95.90	23.0	5.9	62	55	7	312	27	219	293	19	70	134	72	97	C13	Thrust
507	6/2/2006	12:40:40.9	2.59	95.88	29.2	4.8	9	71	21	338	67	182	185	41	−56	323	57	−116	C13	Normal
508	6/2/2006	23:55:13.9	1.42	96.87	25.0	5.2	60	23	9	128	28	223	336	19	119	126	74	81	C13	Thrust
509	1/3/2006	14:36:4.8	2.62	95.44	26.2	5.0	64	76	1	344	26	254	341	19	87	164	71	91	C13	Thrust
510	4/4/2006	10:36:59.7	0.36	97.22	12.0	5.2	23	53	15	317	62	196	171	26	−52	311	70	−106	C13	Normal
511	25/4/2006	18:26:21.4	1.78	96.77	12.0	6.4	51	50	3	317	39	225	293	7	66	137	84	93	C13	Thrust
512	9/5/2006	3:25:26.2	1.02	97.05	24.0	4.9	67	11	10	126	20	220	328	26	114	122	66	79	C13	Thrust
513	21/11/2007	3:30:15	2.81	96.19	41.0	4.9	69	2	10	119	18	212	318	28	111	114	64	79	C13	Thrust
514	21/11/2007	3:30:15	2.81	96.19	41.0	4.9	69	2	10	119	18	212	318	28	111	114	64	79	C13	Thrust
515	22/12/2007	12:26:21.3	1.92	96.58	25.0	6.1	53	55	4	320	37	227	295	9	65	141	82	94	C13	Thrust
516	22/1/2008	17:15:1.8	0.87	97.18	23.0	6.2	62	42	4	140	28	232	332	17	103	138	73	86	C13	Thrust
517	24/1/2008	12:4:20.7	0.92	97.01	24.5	5.3	67	34	5	136	23	228	328	23	103	134	68	85	C13	Thrust
518	20/2/2008	8:8:45.4	2.69	95.98	14.9	7.3	56	42	2	309	34	218	299	11	80	130	79	92	C13	Thrust

Table 4. Composite CMT solutions for the Burmese–Andaman and West Sunda Arc system (reference figures 6–8).

Cluster no	T axis		P axis		Nodal fault plane 1		Nodal fault plane 2
	Plunge	Azimuth	Plunge	Azimuth	Strike	Dip and dip direction	Strike	Dip and dip direction
Map (refer figs 6a–8a)
C4, C5, C6	64°	86° N	24°	266° N	8° N	29° E	190° N	60° W
C7, C8	12°	344° N	79°	151° N	73° N	33° SE	252° N	55° NW
C9	16°	109° N	24°	6° N	54° N	86° SE	146° N	62° SW
C10, C11, C12, C13	75°	46° N	25°	225° N	132° N	64° SW	319° N	25° NE
Section (reference figures 8(b) and 8(e))
A	68°	37° N	22°	229° N	335° N	26° NE	135° N	66° SW
B	73°	32° N	15°	226° N	325° N	30° E	131° N	61° SW
C	65°	46° N	24°	219° N	303° N	19° NE	132° N	71° SW
D	66°	40° N	24°	224° N	320° N	22° NE	131° N	69° SW

The right-lateral strike-slip motion in both the plates is consistent with the geometry in Burmese arc and surrounding terrains in China where right-lateral strike-slip movement predominates along N–S to NW–SE planes. The motion of the Indian plate is primarily accommodated by the positive slips associated with the thrust movement along EBT zones resulting in formation of C2 and C3 clusters. The counter motion on the overriding plate generates the cluster C1. The residual slip adjustment takes place along the Shan-Sagaing fault that principally accommodates a sizeable amount of the motion by aseismic slip/creep along its length up to the Gulf of Martaban and may have contributed to the extension along ASR.

4.2 Andaman Arc Clusters: C4–C8

Seismic clusters C4, C5 and C6 underlie the Andaman fore arc; they are thrust-dominated clusters with normal fault events (figure 7(a)). These shallow focus thrust and normal fault events have predominantly been generated by bending of the subducting Indian Plate and occurred at the leading edge of the subduction zone and the trench where the Indian plate descends. The concentration of strike-slip events in the northern extremity of C4 cluster indicates the strike-slip movement along the adjacent mantle penetrating hinge fault. Clusters C7 and C8 found below the ASR exhibit predominantly normal and subordinate strike-slip events that illustrate the basic tectonic pattern under the spreading arc. The strain partitioning in terms of normal and strike-slip movement demonstrate dyke intrusion, spreading, rift formation and collapse of rift wall, rift-related volcanism and generation of earthquake swarms along ASR (Mukhopadhyay and Dasgupta 2008). The composite CMT plot of C4, C5 and C6 clusters disposed parallel to the Andaman trench shows thrust movement along N–S-oriented thrust planes dipping ∼30° easterly (figure 7(a)). Both compression and tensional directions are oriented E–W where compression prevails at a shallower angle (24°), while extension is taken up at higher angle (64°). This situation gets reversed at C7–C8 clusters along ASR where overall strain partitioning is normal along ENE–WSW-oriented planes. Overall compression is at a high angle (79°) along NW–SE, whereas extension dominates at a shallower angle (12°) along a NNW–SSE direction (table 4). The tectonics along clusters C7 and C8 is represented by penetration of crustal scale faults inside the hot mantle along the upper plate, influence of branches of Kerguelen plume, magmatic dyke intrusion, rifting and spreading that have been taken place for last 4 Ma. The cluster has a shallow depth connotation up to 30 km, which by itself is suggestive of the presence of an upwelling hot mantle underneath it.

4.3 South Andaman Sea Cluster C9

This large cluster has almost equal numbers of normal and strike-slip events. The distribution of both strike-slip and normal fault events in this cluster zone actually corresponds to a complex faulting episode: normal faulting for the rift zone and strike-slip movements for its transgressive regional faults. This cluster is found in the area where a swarm of events originated within a span of only 6 days between 26 and 31 January 2005, following the occurrence of the great Andaman earthquake (M _w 9.3) of 26 December 2004. The analysis and supporting evidence suggest that the earthquakes in this cluster are generated by intruding magmatic dykes along the weak zones in the crust, followed by rifting, spreading and collapse of rift walls (Mukhopadhyay and Dasgupta 2008). Magma injection in rifted areas commonly invokes the injection of shallow, vertical, en-echelon dykes extending along a narrow rift zone, and this injection accounts for the initial strike-slip motion followed by the collapse of the closely spaced inner rift wall with earthquakes of a normal fault source mechanism (Hill 1977). Similarly, CMT solutions for 2005 swarm activity indicate that intrusion of magmatic dyke in the crustal weak zone is documented by earthquakes showing a strike-slip solution. Subsequent events with a normal fault mechanism corroborate the rift formation, collapse and its spread. The overall composite CMT plot (figure 8(c)) indicates a major strike-slip motion with an appreciable normal component along a steep-dipping (86°) NE–SW plane. Both compressional and tensional axes make a shallow angle (24–16°) along the N–S and ESE–WNW directions respectively (table 4). The composite plot along the WAF shows primarily a normal with right-lateral strike-slip component along a steep dipping NE–SW trending surface in the overriding upper plate. Based on evidence from seismology, bathymetry, gravity, time-dependent pore pressure perturbations, rift-related volcanism and calculations on phases of rifting, we assume that a nascent rift is in the process of formation at this location (Mukhopadhyay and Dasgupta 2008, Mukhopadhyay et al. 2010). The orientation of the nascent rift is perpendicular to the regional trend of strike-slip faults of WAF and SFS.

4.4 Offshore Sumatra Clusters: C10–C13

This is by far the largest and most active seismic zone in the whole region. This zone contains the aftershocks of two great earthquakes of recent times (Sumatra–Andaman earthquake M _w 9.3 of 26 December 2004 and Banyak Island earthquake M _w 8.7 of 28 March 2005). The zone (figure 9(a)) is almost exclusively dominated by earthquakes of thrust mechanisms, related to the underthrusting of the Indian plate below the Sunda Arc and also from the overriding SE Asian Plate. The overall orientation of the thrust planes derived from the composite CMT plot is NW–SE dipping 25° north-easterly (figure 9(a), table 4). P–T axes are orientated NE–SW in close correspondence to the structural disposition of the arc geometry. The concentrations of normal fault-related earthquakes in the longitudinal ends of otherwise thrust-dominated cluster C13 are probably indicative of severe gravity adjustments following the thrusting events. The association of earthquakes belonging to both subducting and overriding plates to create the clusters will be discussed in detail in the following section.

In this section, cluster C10 consists of two clusters A and B (figure 9(b), table 4). These two clusters belong to the Indian and SE Asian plates. The strain partitioning and stress distribution is similar in both these clusters depicting consistent thrust motion along the NW–SE plane (parallel to arc disposition) dipping less than 30° north-easterly. Such consistent thrust plane geometries along subducting and overriding plates is also noticed in the depth section following the largest cluster C13 in this belt (figure 9(e)). The depth section across cluster C13 shows that it contains two clusters C (subducting Indian plate cluster) and D (overriding SE Asian plate cluster). Both these clusters have thrust-dominated movement along the NW–SE striking plane dipping less than 22° towards the north-east parallel to WSA.

Similar geometry and stress partitioning in both the plates in clusters C10 and C13 indicate high seismic coupling, with the extreme compressive nature of this zone resulting from slow subduction of the old Indian plate (Stein and Okal 2007). Here, a noticeable feature is the absence of trench parallel strike-slip motion that is otherwise so prominent along the entire belt. The fault unclamping along shallow dipping thrust planes (<30°) resulted in the Sumatra–Andaman earthquake of 2004 (M _w 9.3) and Banyak Island earthquake of 2005 (M _w 8.7) on either side of the cluster C13 without altering the fault zone frictional condition (Bilek 2007), having a sharp boundary of separation of aftershocks (Engdahl et al. 2007) along a NNE–SSW ridge that acts as a separator (Franke et al. 2008). The two earthquakes have a different strain release pattern (Dewey et al. 2007). The high seismic coupling breaks down northward in between C10 and C9 (figure 4) due to the very buoyant warm crust towards the north (from the tomographic results of Shapiro et al. 2008) where the strike-slip component is dominant again. The zone also indicates probable crustal heterogeneity as indicated by differential slip along the rupture plane recorded along the arc during the rupture propagation of the 2004 Andaman Earthquake (Subarya et al. 2006, Banerjee et al. 2007, Rhie et al. 2007). From cluster C9 northward, under the Andaman frontal arc region, the oblique component of plate motion predominates due to a probable influence of the aseismic 90° E Ridge on the Indian Plate (Gahalaut et al. 2010), whereas south to it, compressive components of the thrust realm predominate, as indicated in the present study. This inference prompts us to believe that future mega-thrust events (with potential to generate a tsunami in the Indian Ocean) will only be restricted in between the clusters C10 and C13. The potentiality of this zone to generate a tsunamogenic earthquake is also discussed elsewhere (Fujii and Satake 2007, Hébert et al. 2007) along with physical records of tsunami from the last 1000 years (Monecke et al. 2008). The clusters and intervening zone between C1 and C10 may spawn moderate magnitude earthquakes resulting from either strike-slip or normal movement. The occurrence of one major earthquake on 11.8.2009 (m _b 7.6; latitude 14.013: longitude 92.923) as a slab bending event with a normal fault plane solution (NEIC) north of north Andaman Island attests this conclusion.

5 Seismic potentiality of the large clusters

Seismic potentiality in terms of maximum earthquake size and predictable crustal movement associated with the five large clusters discussed in the foregoing, namely C2, C8, C9, C10 and C13, are attempted here. The purpose of this analysis is to make a statistical inference on the probable size of an earthquake expected from the large clusters. This is done using an approach discussed by Wells and Coppersmith (1994). The analysis is based on the length of the major axis of a cluster already derived (table 2) and by treating it as the ‘potential rupture length’ to predict the earthquake size depending on the type of movement–strike-slip or thrust.

Maximum seismic potentiality is inferred for cluster C13 that may spawn an earthquake of estimated size M _w 8.8, with a rupture length of 460 km, having an anticipated thrust movement. In fact, this zone of seismic cluster has generated two mega-earthquakes in the recent past: Sumatra–Andaman earthquake M _w 9.3 of 26 December 2004 and the Banyak Island earthquake M _w 8.7 of 28 March 2005. Similarly, clusters C2 and C10 with a thrust affinity can generate earthquakes of maximum magnitude M _w 7.9 and 8.2, whereas C8 and C9 may generate earthquakes of M _w 7.6 and 8.2, respectively.

6 Conclusions

The seismicity map and its correlation to crustal and mantle faults for the BAAS and WSA are given in this study. For this, only 1752 events of m _b  =  5.0 and above are selected, using frequency–magnitude relationships, from an earthquake catalogue of 13,057 events, spread over more than a century. The selected events constitute barely 14% of the entire dataset. A cluster analysis using the methodology discussed in this study brings out 13 clusters distributed in different segments of the arc system. Nearly half the earthquake population below the arc is actually confined to these clusters that have a linear fractal geometry consistent with the traces of seismogenic surfaces. Correlation of clusters to seismological depth sections and the result derived from 518 CMT solutions of earthquakes reveals details on the distribution of stress axes, their variation between the individual clusters and the corresponding faulting pattern. With the exception of the back-arc seismicity (clusters C7 and C8), the clusters correspond closely with the thrust planes under the fore-arc. Epicentres in clusters are much shallower, only 50 km (except C2 and C3), for BAAS and within 100 km for WSA. Moreover, the cluster in the western part (C12) of WSA is of a shallower depth of 30–40 km. This is interesting and important because clustering of seismicity is confined in both plates: the subducting Indian plate and the overriding Burmese/SE Asian plate. These results provide a composite three-dimensional perspective on the stress distribution between the clustered seismic zones of the arc and their relationship to focal depths. We have argued elsewhere that a nascent rift around 8° N latitude skirting the Sewell Seamount in south Andaman Sea shows up as a conspicuous seismic zone (Mukhopadhyay and Dasgupta 2008, Mukhopadhyay et al. 2010) (figure 4). It is interesting to note that this is situated near the present Cluster 9 in front of the Andaman subduction zone. The seismic potentiality of the clusters reveals that clusters C2, C8, C9, C10 and C13 may generate earthquakes varying from M _w 7.6 to 8.8.

Acknowledgements

The authors are grateful to the two reviewers for their comments/suggestions which have helped to improve the earlier version of the manuscript.