Sequential Indicator Simulations maps of porosity, depth and thickness of Miocene clastic sediments in the Kloštar field, Northern Croatia

Figures & data

Figure 1. Kloštar Field location (Velić et al., 2011)

Figure 2. Chrono- and lithostratigraphy overview for SE margin of the Pannonian Basin System (modified after Malvić & Cvetković, 2013).

Table 1. Analyzed variables values of the reservoir ‘A’ of the Kloštar Field.

Well	Porosity (%)	Thickness (m)
K-1	19.9	13.0
K-2	19.5	12.0
K-3	19.6	12.0
K-4	21.1	13.0
K-5	23.3	11.5
K-6	20.5	12.0
K-7	20.1	11.0
K-8	21.2	9.5
K-9	17.9	20.0
K-10	19.2	17.0
K-11	13.8	3.0
K-12	5.5	4.5
K-13	19.7	13.5
K-14	18.2	25.0
K-15	21.8	6.0
K-16	18.1	9.0
K-17	18.5	10.0
K-18	19.6	11.0
K-19	22.0	8.0
K-20	18.4	6.0

Velić , J. , Malvić , T. and Cvetković , M. 2011 . Palinspastic reconstruction of synsedimentary tectonics of Neogene and Quaternary sediments in the Kloštar Field (Sava Depression, Pannonian Basin, Croatia) . Zeitschrift der Deutschen Gesellschaft für Geowissenschaften , 162 ( 2 ) : 193 – 203 . (doi:10.1127/1860-1804/2011/0162-0193)

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Malvić , T. and Cvetković , M. 2013 . Lithostratigraphic units in the Drava Depression (Croatian and Hungarian parts) – a correlation . Nafta , 64 ( 1 ) : 27 – 33 .

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