Geochemical characteristics of ophiolitic rocks from the southern margin of the Sivas basin and their implications for the Inner Tauride Ocean, Central-Eastern Turkey

References

• Alabaster, T., Pearce, J. A., & Malpas, J. (1982). The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex. Contributions to Mineralogy and Petrology, 81, 168–183.10.1007/BF00371294
   Web of Science ®Google Scholar
• Aldanmaz, E., Schmidt, M. W., Gourgaud, A., & Meisel, T. (2009). Mid-ocean ridge and supra-subduction geochemical signatures in spinel-peridotites from the Neotethyan ophiolites in SW Turkey: Implications for upper mantle melting processes. Lithos, 113, 691–708.10.1016/j.lithos.2009.03.010
   Web of Science ®Google Scholar
• Al-Riyami, K., Robertson, A. H. F., Dixon, J., & Xenophontos, C. (2002). Origin and emplacement of the Late Cretaceous Baer-Bassit ophiolite and its metamorphic sole in NW Syria. Lithos, 65, 225–260.10.1016/S0024-4937(02)00167-6
   Web of Science ®Google Scholar
• Andrew, T., & Robertson, A. H. F. (2002). The Beyşehir-Hoyran-Hadim Nappes: Genesis and emplacement of Mesozoic marginal and oceanic units of the northern Neotethys in southern Turkey. Journal of the Geological Society, 159, 529–543.10.1144/0016-764901-157
   Web of Science ®Google Scholar
• Arculus, R. J., & Powell, R. (1986). Source component mixing in the regions of arc magma generation. Journal of Geophysical Research, 91, 5913–5926.10.1029/JB091iB06p05913
   Web of Science ®Google Scholar
• Atabey, E., & Aktimur, H. T. (1997). 1:100.000 geological map of Turkey. 48, (Sivas-G24). Ankara: MTA.
   Google Scholar
• Bağcı, U., & Parlak, O. (2009). Petrology of the Tekirova (Antalya) ophiolite (Southern Turkey): Evidence for diverse magma generations and their tectonic implications during Neotethyan-subduction. International Journal of Earth Sciences, 98, 387–405.
   Web of Science ®Google Scholar
• Bağcı, U., Parlak, O., & Höck, V. (2005). Whole rock and mineral chemistry of cumulates from the Kızıldağ (Hatay) ophiolite (Turkey): Clues for multiple magma generation during crustal accretion in the southern Neotethyan ocean. Mineralogical Magazine, 69, 53–76.
   Web of Science ®Google Scholar
• Bağcı, U., Parlak, O., & Höck, V. (2006). Geochemical character and tectonic environment of ultramafic to mafic cumulates from the Tekirova (Antalya) ophiolite (southern Turkey). Geological Journal, 41, 193–219.
   Web of Science ®Google Scholar
• Bağcı, U., Parlak, O., & Höck, V. (2008). Geochemistry and tectonic environment of diverse magma generations forming the crustal units of the Kızıldağ (Hatay) ophiolites southern Turkey. Turkish Journal of Earth Sciences, 17, 43–71.
   Web of Science ®Google Scholar
• Ballhaus, C. (1993). Redox states of lithospheric and asthenospheric upper mantle. Contributions to Mineralogy and Petrology, 114, 331–348.10.1007/BF01046536
   Web of Science ®Google Scholar
• Beard, J. S. (1986). Characteristic mineralogy of arc-related cumulate gabbros: Implications for the tectonic setting of gabbroic plutons and for andesite genesis. Geology, 14, 848–851.10.1130/0091-7613(1986)14<848:CMOACG>2.0.CO;2
   Web of Science ®Google Scholar
• Beccaluva, L., Coltorti, M., Giunta, G., & Siena, F. (2004). Tethyan vs. Cordilleran ophiolites: A reappraisal of distinctive tectono-magmatic features of supra-subduction complexes in relation to the subduction mode. Tectonophysics, 393, 163–174.10.1016/j.tecto.2004.07.034
   Web of Science ®Google Scholar
• Beccaluva, L., Coltorti, M., Saccani, E., & Siena, F. (2005). Magma generation and crustal accretion as evidenced by supra-subduction ophiolites of the Albanide-Hellenide Subpelagonian zone. The Island Arc, 14, 551–563.10.1111/iar.2005.14.issue-4
   Web of Science ®Google Scholar
• Caran, Ş., Çoban, H., Flower, M. F. J., Ottley, C. J., & Yılmaz, K. (2010). Podiform chromitites and mantle peridotites of the Antalya ophiolite, Isparta Angle (SW Turkey): Implications for partial melting and melt-rock interaction in oceanic and subduction-related settings. Lithos, 114, 307–326.10.1016/j.lithos.2009.09.006
   Web of Science ®Google Scholar
• Çelik, Ö. F. (2007). Metamorphic sole rocks and their mafic dykes in the eastern Tauride belt ophiolites (southern Turkey): İmplications for OIB type magma generation following slab break-off. Geological Magazine, 144, 849–866.
   Web of Science ®Google Scholar
• Çelik, Ö. F. (2008). Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, southern Turkey. Turkish Journal of Earth Sciences, 17, 685–708.
   Web of Science ®Google Scholar
• Çelik, Ö. F., & Chiaradia, M. (2008). Geochemical and petrological aspects of dyke intrusions in the Lycian ophiolites (SW Turkey): A case study for the dyke emplacement along the Tauride Belt Ophiolites. International Journal of Earth Sciences, 97, 1151–1164.
   Web of Science ®Google Scholar
• Çelik, Ö. F., & Delaloye, M. (2003). Origin of metamorphic soles and their post-kinematic mafic dyke swarms in the Antalya and Lycian ophiolites, SW Turkey. Geological Journal, 38, 235–256.
   Web of Science ®Google Scholar
• Çelik, Ö. F., Delaloye, M., & Feraud, G. (2006). Precise 40Ar-39Ar ages from the metamorphic sole rocks of the Tauride Belt Ophiolites, southern Turkey: İmplications for the rapid cooling history. Geological Magazine, 143, 213–227.
   Web of Science ®Google Scholar
• Çelik, Ö. F., Marzoli, A., Marschik, R., Chiaradia, M., Neubauer, N., & Öz, İ. (2011). Early-middle Jurassic intraoceanic subduction in the İzmir-Ankara-Erzincan Ocean, northern Turkey. Tectonophysics, 509, 120–134.
   Web of Science ®Google Scholar
• Çetinkaplan, M., Pourteau, A., Candan, O., Koralay, O. E., Oberhänsli, R., Okay, A. I., … Şengün, F. (2016). P-T-t evolution of eclogite/blueschist facies metamorphism in Alanya Massif: Time and space relations with HP event in Bitlis Massif, Turkey. International Journal of Earth Sciences, 105, 247–281.10.1007/s00531-014-1092-8
   Web of Science ®Google Scholar
• Clark, M., & Robertson, A. H. F. (2002). The role of the Early Tertiary Ulukisla Basin, southern Turkey, in suturing of the Mesozoic Tethys ocean. Journal of the Geological Society, 159, 673–690.10.1144/0016-764902-015
   Web of Science ®Google Scholar
• Collins, A. S., & Robertson, A. H. F. (1997). Lycian melange, southwestern Turkey: An emplaced Late Cretaceous accretionary complex. Geology, 25, 255–258.10.1130/0091-7613(1997)025<0255:LMSTAE>2.3.CO;2
   Web of Science ®Google Scholar
• Collins, A. S., & Robertson, A. H. F. (1998). Processes of Late Cretaceous to Late Miocene episodic thrust sheet translation in the Lycian Taurides, SW Turkey. Journal of the Geological Society, 155, 759–772.10.1144/gsjgs.155.5.0759
   Web of Science ®Google Scholar
• Collins, A. S., & Robertson, A. H. F. (1999). Evolution of the Lycian Allochthon, western Turkey, as a North-facing Late Palaeozoic to Mesozoic rift and passive continental margin. Geological Journal, 34, 107–138.10.1002/(ISSN)1099-1034
   Web of Science ®Google Scholar
• Dilek, Y., & Flower, M. F. J. (2003). Arc-trench rollback and forearc accretion: 2. A model template for Ophiolites in Albania, Cyprus, and Oman. In Y. Dilek, & P. T. Robinson (Eds.), Ophiolites in Earth history (Vol. 218, pp. 43–68). London: Geological Society, Special Publications.
   Google Scholar
• Dilek, Y., & Thy, P. (2006). Age and petrogenesis of plagiogranite intrusions in the Ankara melange, central Turkey. Island Arc, 15, 44–57.10.1111/iar.2006.15.issue-1
   Web of Science ®Google Scholar
• Dilek, Y., & Thy, P. (2009). Island arc tholeiite to boninitic melt evolution of the Cretaceous Kizildag (Turkey) ophiolite: Model for multi-stage early arc–forearc magmatism in Tethyan subduction factories. Lithos, 113, 68–87.10.1016/j.lithos.2009.05.044
   Web of Science ®Google Scholar
• Dilek, Y., & Whitney, D. L. (1997). Counterclockwise P-T-t trajectory from the metamorphic sole of a Neo-Tethyan ophiolite (Turkey). Tectonophysics, 280, 295–310.10.1016/S0040-1951(97)00038-3
   Web of Science ®Google Scholar
• Dilek, Y., Thy, P., Hacker, B. R., & Grundvig, S. (1999). Structure and petrology of Tauride ophiolites and mafic dike intrusions (Turkey): Implications for the Neotethyan ocean. Geological Society of America Bulletin, 111, 1192–1216.10.1130/0016-7606(1999)111<1192:SAPOTO>2.3.CO;2
   Web of Science ®Google Scholar
• Dilek, Y., Furnes, H., & Shallo, M. (2008). Geochemistry of the Jurassic Mirdita Ophiolite (Albania) and the MORB to SSZ evolution of a marginal basin oceanic crust. Lithos, 100, 174–209.10.1016/j.lithos.2007.06.026
   Web of Science ®Google Scholar
• Droop, G. T. R., Karakaya, M. C., Eren, Y., & Karakaya, N. (2005). Metamorphic evolution of blueschists of the Altınekin Complex, Konya area, south central Turkey. Geological Journal, 40, 127–153.10.1002/(ISSN)1099-1034
   Web of Science ®Google Scholar
• Elitok, Ö. (2001). Geochemistry and tectonic significance of the Şarkikaraağaç ophiolites in the Beyşehir-Hoyran Nappes, SW Turkey. In Ö. Akıncı, M. Görmüş, M. Kuşçu, R. Karagüzel, & M. Bozcu (Eds.), Proceedings of the 4th International Symposium on Eastern Mediterranean Geology, 21–25 May 2001 Isparta, Turkey, pp. 181–196.
   Google Scholar
• Elitok, Ö., & Drüppel, K. (2008). Geochemistry and tectonic significance of metamorphic sole rocks beneath the Beyşehir-Hoyran ophiolite (SW-Turkey). Lithos, 100, 322–353.10.1016/j.lithos.2007.06.022
   Web of Science ®Google Scholar
• Fayon, A. K., Whitney, D. L., Teyssier, C., Garver, J. I., & Dilek, Y. (2001). Effects of plate convergence obliquity on timing and mechanisms of exhumation of a mid-crustal terrain, the Central Anatolian Crystalline Complex. Earth and Planetary Science Letters, 192, 191–205.10.1016/S0012-821X(01)00440-X
   Web of Science ®Google Scholar
• Floyd, P. A., & Winchester, J. A. (1978). Identification and discrimination of altered and metamorphosed volcanic rocks using immobile elements. Chemical Geology, 21, 291–306.10.1016/0009-2541(78)90050-5
   Web of Science ®Google Scholar
• Gökten, E. (1993). Geology of the southern boundary of the Sivas Basin in the east of Ulaş (Sivas–central Anatolia): Tectonic development related to the closure of inner Tauride Ocean. Turkish Association of Petroleum Geologist Bulletin, 5, 35–55.
   Google Scholar
• Gökten, E., & Floyd, P. A. (1987). Geochemistry and tectonic environment of the Şarkışla area volcanic rocks in Central Anatolia, Turkey. Mineralogical Magazine, 51, 553–559.10.1180/minmag
   Web of Science ®Google Scholar
• Göncüoğlu, M. C., Özcan, A., Turhan, N., & Işık, A. (1992). Stratigraphy of the Kütahya region. ISGB-92. Field Guide Book 3. Ankara, Turkey: MTA.
   Google Scholar
• Göncüoğlu, M. C., Dirik, K., & Kozlu, H. (1996–1997). Pre-alpine and alpine terranes in Turkey: Explanatory notes to the terrane map of Turkey. Annalles Geologiques des Pays Hellenique, 37, 1–3.
   Google Scholar
• Görür, N., Oktay, F. Y., Seymen, İ., & Şengör, A. M. C. (1984). Palaeotectonic evolution of the Tuzgölü basin complex, Central Turkey: Sedimentary record of a Neotethyan closure. In J. A. Dixon, & A. H. F. Robertson (Eds.), The Geological Evolution of the Eastern Mediterranean (Vol. 17, pp. 467–482). London: Geological Society, Special Publications.
   Google Scholar
• Görür, N., Tüysüz, O., & Şengör, A. M. C. (1998). Tectonic evolution of the central Anatolian basins. International Geology Review, 40, 831–850.
   Web of Science ®Google Scholar
• Gust, D. A., & Johnson, R. W. (1981). Amphibole bearing cumulates from Boisa island, Papua New Guinea: Evaluation of the role of fractional crystallization in an andesitic volcano. Journal of Geology, 89, 219–232.10.1086/628581
   Web of Science ®Google Scholar
• Hall, C. E., Gurnis, M., Sdrolias, M., Lavier, L. L., & Müller, R. D. (2003). Catastrophic initiation of subduction following forced convergence across fracture zones. Earth and Planetary Science Letters, 212, 15–30.10.1016/S0012-821X(03)00242-5
   Web of Science ®Google Scholar
• Hart, S. R., Erlank, A. J., & Kable, E. J. D. (1974). Sea floor basalt alteration: Some chemical and Sr isotopic effects. Contributions to Mineralogy and Petrology, 44, 219–230.10.1007/BF00413167
   Web of Science ®Google Scholar
• van Hinsbergen, D. J. J., Maffione, M., Plunder, A., Kaymakcı, N., Ganerød, M., Hendriks, B. W. H., … Vissers, R. L. M. (2016). Tectonic evolution and paleogeography of the Kırşehir Block and the Central Anatolian Ophiolites, Turkey. Tectonics, 35, 983–1014.10.1002/tect.v35.4
   Web of Science ®Google Scholar
• Humphris, S. E., & Thompson, G. (1978). Trace element mobility during hydrothermal alteration of oceanic basalts. Geochimica et Cosmochimica Acta, 42, 127–136.10.1016/0016-7037(78)90222-3
   Web of Science ®Google Scholar
• İnan, S., & İnan, N. (1987). Tecer kireçtaşı formasyonunun stratigrafik tanımlanması. Cumhuriyet Üniversitesi Mühendislik Fakültesi Dergisi, Yerbilimleri, 4, 13–22.
   Google Scholar
• Ishizuka, O., Tani, K., Reagan, M. K., Kanayama, K., Umino, S., Harigane, Y., … Dunkley, D. J. (2011). The timescales of subduction initiation and subsequent evolution of an oceanic island arc. Earth and Planetary Science Letters, 306, 229–240.10.1016/j.epsl.2011.04.006
   Web of Science ®Google Scholar
• Jakes, P., & Gill, J. (1970). Rare earth elements and the island arc tholeiitic series. Earth Planetary Science Letters, 9, 17–28.10.1016/0012-821X(70)90018-X
   Web of Science ®Google Scholar
• Jenner, G. A., Dunning, G. R., Malpas, J., Brown, M., & Brace, T. (1991). Bay of Islands and Little Port complexes, revisited: Age, geochemical and isotopic evidence confirm suprasubduction-zone origin. Canadian Journal of Earth Sciences, 28, 1635–1652.10.1139/e91-146
   Web of Science ®Google Scholar
• van der Kaaden, G. (1966). Importance and distribution of glaucophane bearing rocks in Turkey. Maden Tetkik ve Arama Enstitüsü Dergisi, 67, 38–69.
   Google Scholar
• Kadıoğlu, Y. K., Dilek, Y., & Foland, K. A. (2006). Slab breakoff and syncollisional origin of the Late Cretaceous magmatism in the Central Anatolian Crystalline Complex, Turkey. In Y. Dilek, & S. Pavlides (Eds.), Postcollisional tectonics and magmatism in the Mediterranean Region and Asia (Vol. 409, pp. 381–415). Boulder, CO: Geological Society of America Special Paper.
   Google Scholar
• Karaoğlan, F., Parlak, O., Klötzli, U., Thöni, M., & Koller, F. (2012). U-Pb and Sm–Nd geochronology of the ophiolites from the SE Turkey: İmplications for the Neotethyan evolution. Geodinamica Acta, 25, 146–161.10.1080/09853111.2013.858948
   Web of Science ®Google Scholar
• Karaoğlan, F., Parlak, O., Klötzlı, U., Thönı, M., & Koller, F. (2013). U-Pb and Sm-Nd geochronology of the Kızıldağ (Hatay, Turkey) ophiolite: İmplications for the timing and duration of suprasubduction zone type oceanic crust formation in the southern Neotethys. Geological Magazine, 150, 283–299.10.1017/S0016756812000477
   Web of Science ®Google Scholar
• Karaoğlan, F., Parlak, O., Klötzli, U., Koller, F., & Rızaoğlu, T. (2013). Age and duration of intra-oceanic arc volcanism built on a suprasubduction zone type oceanic crust in southern Neotethys, SE Anatolia. Geoscience Frontiers, 4, 399–408.10.1016/j.gsf.2012.11.011
   Web of Science ®Google Scholar
• Kavak, K. Ş. (2010). Sivas havzası güney kenarının ASTER uydu görüntüleriyle incelenmesi ve spektral kütüphanesinin oluşturulması. Tübitak projesi, 107Y146, 128 pp
   Google Scholar
• Kelley, K. A., & Cottrell, E. (2012). The influence of magmatic differentiation on the oxidation state of Fe in a basaltic arc magma. Earth and Planetary Science Letters, 329–330, 109–121.10.1016/j.epsl.2012.02.010
   Web of Science ®Google Scholar
• Koglin, N. (2008). Geochemistry, petrogenesis and tectonic setting of Ophiolites and mafic-ultramafic complexes in the Northeastern Aegean Region: New trace-element, isotopic and age constraints (Unpublished doctoral dissertation). Mainz, Germany.
   Google Scholar
• Koglin, N., Kostopoulos, D., & Reischmann, T. (2009). Geochemistry, petrogenesis and tectonic setting of the Samothraki mafic suite, NE Greece: Trace-element, isotopic and zircon age constraints. Tectonophysics, 473, 53–68.10.1016/j.tecto.2008.10.028
   Web of Science ®Google Scholar
• Konstantinou, A., Wirth, K. R., & Vervoort, J. (2007). U-Pb isotopic dating of Troodos plagiogranite, Cyprus by LA-ICP-MS. GSA Annual Meeting, Geological Society of America, Abstracts with Programs, 39, 388.
   Google Scholar
• Liati, A., Gebauer, D., & Fanning, C. M. (2004). The age of ophiolitic rocks of the Hellenides (Vourinos, Pindos, Crete): First U-Pb ion microprobe (SHRIMP) zircon ages. Chemical Geology, 207, 171–188.10.1016/j.chemgeo.2004.02.010
   Web of Science ®Google Scholar
• Lytwyn, J. N., & Casey, J. F. (1995). The geochemistry of postkinematic mafic dike swarms and subophiolitic metabasites, Pozanti-Karsanti ophiolite, Turkey: Evidence for ridge subduction. Geological Society of America Bulletin, 107, 830–850.10.1130/0016-7606(1995)107<0830:TGOPMD>2.3.CO;2
   Web of Science ®Google Scholar
• Meffre, S., Aitchison, J., & Crawford, A. J. (1996). Geochemical evolution and tectonic significance of boninites and tholeiites from the Koh ophiolite, New Caledonia. Tectonics, 15, 67–83.10.1029/95TC02316
   Web of Science ®Google Scholar
• MTA. (2002). 1:500.000 ölçekli Türkiye jeoloji haritası [Geological map of Turkey, 1:500.000]. Ankara: MadenTektik ve Arama Genel Müdürlüğü [General Directorate of Mineral Research and Exploration].
   Google Scholar
• Mukasa, S. B., & Ludden, J. N. (1987). Uranium-lead isotopic ages of plagiogranites from the Troodos ophiolite, Cyprus, and their tectonic significance. Geology, 15, 825–828.10.1130/0091-7613(1987)15<825:UIAOPF>2.0.CO;2
   Web of Science ®Google Scholar
• Okay, Aİ. (1982). Incipient blueschist metamorphism and metasomatism in the Tavşanlı Region, northwest Turkey. Contributions to Mineralogy and Petrology, 79, 361–367.10.1007/BF01132065
   Web of Science ®Google Scholar
• Okay, Aİ., & Tüysüz, O. (1999). Tethyan sutures of northern Turkey. In A. Mascle, & L. Jolivet (Eds.), The Mediterranean basins: Tertiary extension within the Alpine Orogeny (Vol. 156, pp. 475–516). London: Geological Society, Special Publications.
   Google Scholar
• Okay, Aİ., Harris, N. B. W., & Kelley, S. (1998). Exhumation of blueschists along a Tethyan suture in northwest Turkey. Tectonophysics, 285, 275–299.10.1016/S0040-1951(97)00275-8
   Web of Science ®Google Scholar
• Parlak, O. (1996). Geochemistry and geochronology of the Mersin ophiolite within the Eastern Mediterranean tectonic frame (Southern Turkey) (Unpublished doctoral dissertation). University of Geneva, Switzerland.
   Google Scholar
• Parlak, O. (2000). Geochemistry and significance of mafic dyke swarms in the Pozantı-Karsantı ophiolite (southern Turkey). Turkish Journal of Earth Sciences, 24, 29–38.
   Google Scholar
• Parlak, O. (2016). The Tauride ophiolites of Anatolia (Turkey): A review. Journal of Earth Science, 27, 901–934.10.1007/s12583-016-0679-3
   Web of Science ®Google Scholar
• Parlak, O., & Delaloye, M. (1996). Geochemistry and timing of post-metamorphic dyke emplacement in the Mersin ophiolite (southern Turkey): New age constraints from 40Ar/39Ar geochronology. Terra Nova, 8, 585–592.10.1111/ter.1996.8.issue-6
   Web of Science ®Google Scholar
• Parlak, O., & Delaloye, M. (1999). Precise 40Ar/39Ar ages from the metamorphic sole of the Mersin ophiolite (southern Turkey). Tectonophysics, 301, 145–158.10.1016/S0040-1951(98)00222-4
   Web of Science ®Google Scholar
• Parlak, O., & Robertson, A. H. F. (2004). The ophiolite-related Mersin Melange, southern Turkey: Its role in the tectonicsedimentary setting of Tethys in the Eastern Mediterranean region. Geological Magazine, 141, 257–286.10.1017/S0016756804009094
   Web of Science ®Google Scholar
• Parlak, O., Delaloye, M., & Bingöl, E. (1995). Origin of subophiolitic metamorphic rocks beneath the Mersin ophiolite, southern Turkey. Ofioliti, 20, 97–110.
   Google Scholar
• Parlak, O., Delaloye, M., & Bíngöl, E. (1996). Mineral chemistry of ultramafic and mafic cumulates as an indicator of the arc-related origin of the Mersin ophiolite (southern Turkey). Geologische Rundschau, 85, 647–661.10.1007/BF02440102
   Google Scholar
• Parlak, O., Höck, V., Kozlu, H., & Delaloye, M. (2004). Oceanic crust generation in an island arc tectonic setting, SE Anatolian orogenic belt (Turkey). Geological Magazine, 141, 583–603.10.1017/S0016756804009458
   Web of Science ®Google Scholar
• Parlak, O., Höck, V., & Delaloye, M. (2000). Suprasubduction zone origin of the Pozanti-Karsanti ophiolite (southern Turkey) deduced from whole-rock and mineral chemistry of the gabbroic cumulates. In E. Bozkurt, J. A. Winchester, & J. D. A. Piper (Eds.), Tectonics and magmatism in Turkey and the surrounding area (Vol. 173, pp. 219–234). London: Geological Society, Special Publications.
   Google Scholar
• Parlak, O., Höck, V., & Delaloye, M. (2002). The suprasubduction Pozanti-Karsanti ophiolite, southern Turkey: Evidence for high pressure crystal fractionation of ultramafic cumulates. Lithos, 65, 205–224.10.1016/S0024-4937(02)00166-4
   Web of Science ®Google Scholar
• Parlak, O., Yılmaz, H., Boztuğ, D., & Höck, V. (2005). Geochemistry and tectonic setting of the Divriği ophiolite in the east central Anatolia (Sivas, Turkey): Evidence for melt generation within an asthenospheric window prior to ophiolite emplacement onto the Taurides. International Symposium on the Geodynamics of Eastern Mediterranean: Active Tectonics of the Aegean Region, 15–18, June 2005. Turkey, İstanbul: Kadir Has University, p. 224.
   Google Scholar
• Parlak, O., Yılmaz, H., & Boztuğ, D. (2006). Geochemistry and tectonic setting of the metamorphic sole rocks and isolated dykes from the Divriği ophiolite (Sivas, Turkey): Evidence for melt generation within an asthenospheric window prior to ophiolite emplacement. Turkish Journal of Earth Sciences, 15, 25–45.
   Web of Science ®Google Scholar
• Parlak, O., Rızaoğlu, T., Bağcı, U., Karaoğlan, F., & Höck, V. (2009). Tectonic significance of the geochemistry and petrology of ophiolites in southeast Anatolia, Turkey. Tectonophysics, 473, 173–187.10.1016/j.tecto.2008.08.002
   Web of Science ®Google Scholar
• Parlak, O., Karaoğlan, F., Rızaoğlu, T., Klötzli, U., Koller, F., & Billor, Z. (2013). U-Pb and 40Ar/39Ar geochronology of the ophiolites and granitoids from the Tauride belt: İmplications for the evolution of the Inner Tauride suture. Journal of Geodynamics, 65, 22–37.10.1016/j.jog.2012.06.012
   Web of Science ®Google Scholar
• Parlak, O., Karaoğlan, F., Rızaoğlu, T., Nurlu, N., Bağcı, U., Höck, V., … Topak, Y. (2013). Petrology of the İspendere (Malatya) ophiolite from the Southeast Anatolia: Implications for the Late Mesozoic evolution of the southern Neotethyan ocean. In A. H. F. Robertson, O. Parlak, & U. C. Ünlügenç (Eds.), Geological development of Anatolia and the Easternmost Mediterranean region (Vol. 372, pp. 219–247). London: Geological Society, Special Publications.
   Google Scholar
• Parlak, O., Çolakoğlu, A., Dönmez, C., Sayak, H., Türkel, A., Yıldırım, N., & Odabaşı, İ. (2013). Geochemistry and tectonic significance of Ophiolites along the İzmir-Ankara-Erzincan suture zone in Northeastern Anatolia. In A. H. F. Robertson, O. Parlak, & U. C. Ünlügenç (Eds.), Geological development of Anatolia and the Easternmost Mediterranean region (Vol. 372, pp. 75–105). London: Geological Society, Special Publications.
   Google Scholar
• Pearce, J. A. (1982). Trace element characteristics of lavas from destructive plate boundaries. In R. S. Thorpe (Ed.), Andesites (pp. 525–548). New York, NY: Wiley.
   Google Scholar
• Pearce, J. A. (1983). Role of the subcontinental lithosphere in magma genesis at active continental margins. In C. J. Hawkesworth, & M. J. Norry (Eds.), Continental basalts and mantle xenoliths (pp. 230–249). Cheshire: Shiva Publishing.
   Google Scholar
• Pearce, J. A. (1996). A users guide to basalt discrimination diagrams. In D. A. Wyman (Ed.), Trace element geochemistry of volcanic rocks: Applications for massive sulphide exploration (Vol. 12, pp. 79–113). St. John’s: Geochemistry, Geological Association of Canada, Short Course Notes.
   Google Scholar
• Pearce, J. A. (2003). Supra-subduction zone ophiolites: The search for modern analogues. In Y. Dilek, & S. Newcomb (Eds.), Ophiolite concept and the evolution of geological thought (Vol. 373, pp. 269–293). Boulder, CO: Geological Society of America Special Paper.10.1130/0-8137-2373-6
   Google Scholar
• Pearce, J. A. (2014). Immobile element fingerprinting of ophiolites. Elements, 10, 101–108.10.2113/gselements.10.2.101
   Web of Science ®Google Scholar
• Pearce, J. A., & Cann, J. R. (1973). Tectonic setting of basic volcanic rocks determined using trace element analyses. Earth and Planetary Science Letters, 19, 290–300.10.1016/0012-821X(73)90129-5
   Web of Science ®Google Scholar
• Pearce, J. A., & Norry, M. J. (1979). Petrogenetic implications of Ti, Zr, Y and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology, 69, 33–47.10.1007/BF00375192
   Web of Science ®Google Scholar
• Pearce, J. A., & Parkinson, I. J. (1993). Trace element models of mantle melting: Application to volcanic arc petrogenesis. In H. M. Pichard, T. Alabaster, N. B. W. Harris, & C. R. Neary (Eds.), Magmatic processes and plate tectonics (Vol. 76, pp. 373–403). London: Geological Society, Special Publications.
   Google Scholar
• Pe-Piper, G., Tsıkouras, B., & Hatzıpanagıotou, K. (2004). Evolution of boninites and island-arc tholeiites in the Pindos Ophiolite, Greece. Geological Magazine, 141, 455–469.10.1017/S0016756804009215
   Web of Science ®Google Scholar
• Polat, A., & Casey, J. F. (1995). A structural record of the emplacement of the Pozanti-Karsanti ophiolite onto the Menderes-Taurus block in the late Cretaceous, eastern Taurides, Turkey. Journal of Structural Geology, 17, 1673–1688.10.1016/0191-8141(95)00061-H
   Web of Science ®Google Scholar
• Polat, A., Casey, J. F., & Kerrich, R. (1996). Geochemical characteristics of accreted material beneath the Pozanti-Karsanti ophiolite, Turkey: Intra-oceanic detachment, assembly and obduction. Tectonophysics, 263, 249–276.10.1016/S0040-1951(96)00026-1
   Web of Science ®Google Scholar
• Pourteau, A., Candan, O., & Oberhänsli, R. (2010). High-pressure metasediments in central Turkey: Constraints on the Neotethyan closure history. Tectonics, 29, TC5004. doi:10.1029/2009TC002650
   Web of Science ®Google Scholar
• Reagan, M. K., Ishizuka, O., Stern, R. J., Kelley, K. A., Ohara, Y., Blichert-Toft, J., … Woods, M. (2010). Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system. Geochemistry Geophysics Geosystems, 11, 1–17.
   Web of Science ®Google Scholar
• Reagan, M. K., McClelland, W. C., Girard, G., Goff, K. R., Peate, D. W., Ohara, Y., & Stern, R. J. (2013). The geology of the southern Mariana fore-arc crust: Implications for the scale of Eocene volcanism in the western Pacific. Earth and Planetary Science Letters, 380, 41–51.10.1016/j.epsl.2013.08.013
   Web of Science ®Google Scholar
• Rimmelé, G. (2003). Structural and metamorphic evolution of the Lycian Nappes and the Menderes Massif (southwest Turkey): Geodynamic implications and correlations with the Aegean Domain (Unpublished doctoral dissertation). Potsdam, Germany.
   Google Scholar
• Rızaoğlu, T., Parlak, O., Höck, V., & İşler, F. (2006). Nature and significance of Late Cretaceous ophiolitic rocks and its relation to the Baskil granitoid in Elazığ region, SE Turkey. In A. H. F. Robertson, & D. Mountrakis (Eds.), Tectonic development of the Eastern Mediterranean region (Vol. 260, pp. 327–350). London: Geological Society, Special Publications.
   Google Scholar
• Robertson, A. H. F. (2002). Overview of the genesis and emplacement of Mesozoic ophiolites in the Eastern Mediterranean Tethyan region. Lithos, 65, 1–67.10.1016/S0024-4937(02)00160-3
   Web of Science ®Google Scholar
• Robertson, A. H. F., & Waldron, J. (1990). Geochemistry and tectonic setting of Late Triassic and Late Jurassic-early Cretaceous basaltic extrusives from the Antalya Complex, SW Turkey. In M. Y. Savaşçın, & A. H. Eronat (Eds.), Proceedings of International Earth Science Congress on Aegean Regions (Vol. 2, pp. 279–299). İzmir, Turkey: Dokuz Eylül University.
   Google Scholar
• Robertson, A. H. F., & Woodcock, N. H. (1981a). Bilelyeri Group, Antalya Complex: Deposition on a Mesozoic passive continental margin, south-west Turkey. Sedimentology, 28, 381–399.10.1111/sed.1981.28.issue-3
   Web of Science ®Google Scholar
• Robertson, A. H. F., & Woodcock, N. H. (1981b). Alakırçay Group, Antalya Complex, SW Turkey: A deformed Mesozoic carbonate margin. Sedimentary Geology, 30, 95–131.10.1016/0037-0738(81)90015-4
   Web of Science ®Google Scholar
• Robertson, A. H. F., & Woodcock, N. H. (1981c). Gödene Zone, Antalya Complex SW Turkey: Volcanism and sedimentation on Mesozoic marginal ocean crust. Geologische Rundschau, 70, 1177–1214.10.1007/BF01820188
   Google Scholar
• Robertson, A. H. F., & Woodcock, N. H. (1982). Sedimentary history of the southwestern segment of the Mesozoic-tertiary Antalya continental margin, southwestern Turkey. Eclogae Geologica Helvetica, 75, 517–562.
   Google Scholar
• Robertson, A. H. F., Parlak, O., & Ustaömer, T. (2009). Melange genesis and ophiolite emplacement related to subduction of the northern margin of the Tauride-Anatolide continent, central and western Turkey. In D. J. J. Vanhinsbergen, M. A. Edwards, & R. Govers (Eds.), Collision and collapse at the Africa-Arabia-Eurasia subduction zone (Vol. 311, pp. 9–66). London: Geological Society, Special Publications.
   Google Scholar
• Robertson, A. H. F., Parlak, O., & Ustaomer, T. (2012). Overview of the Palaeozoic-Neogene evolution of Neotethys in the Eastern Mediterranean region (southern Turkey, Cyprus, Syria). Petroleum Geoscience, 18, 381–404.10.1144/petgeo2011-091
   Web of Science ®Google Scholar
• Robertson, A. H. F., Parlak, O., Metin, Y., Vergili, Ö., Taslı, K., İnan, N., & Soycan, H. (2013). Late Palaeozoic-Cenozoic tectonic development of carbonate platform, margin and oceanic units in the Eastern Taurides, Turkey. In A. H. F. Robertson, O. Parlak, & U. C. Ünlügenç (Eds.), Geological development of Anatolia and the Easternmost Mediterranean region (Vol. 372, pp. 167–218). London: Geological Society Special Publication.
   Google Scholar
• Robertson, A. H. F., Parlak, O., Ustaömer, T., Taslı, K., İnan, N., Dumitrica, P., & Karaoğlan, F. (2013). Subduction, ophiolite genesis and collision history of Tethys adjacent to the Eurasian continental margin: New evidence from the Eastern Pontides, Turkey. Geodinamica Acta, 26, 230–293.10.1080/09853111.2013.877240
   Web of Science ®Google Scholar
• Rollinson, H. R. (1993). Using geochemical data: Evaluation, presentation, Interpretation. New York, NY: Wiley.
   Google Scholar
• Saccani, E., & Photiades, A. (2005). Petrogenesis and tectonomagmatic significance of volcanic and subvolcanic rocks in the Albanide-Hellenide ophiolitic melanges. The Island Arc, 14, 494–516.10.1111/iar.2005.14.issue-4
   Web of Science ®Google Scholar
• Saka, S., Uysal, I., Akmaz, R. M., Kaliwoda, M., & Hochleitner, R. (2014). The effects of partial melting, melt-mantle interaction and fractionation on ophiolite generation: Constraints from the late Cretaceous Pozantı-Karsantı ophiolite, southern Turkey. Lithos, 202–203, 300–316.10.1016/j.lithos.2014.05.027
   Web of Science ®Google Scholar
• Sarıfakıoğlu, E., Dilek, Y., & Uysal, İ. (2012). The Petrogenesis and Geodynamic Significance of Bahçe (Osmaniye) Ophiolite. 5th Geochemistry Symposium (pp. 112–113). Denizli,Turkey,
   Google Scholar
• Seaton, N. C. A., Whitney, D. L., Teyssier, C., Toraman, E., & Heizler, M. T. (2009). Recrystallization of high-pressure marble (Sivrihisar, Turkey). Tectonophysics, 479, 241–253.10.1016/j.tecto.2009.08.015
   Web of Science ®Google Scholar
• Sherlock, S., Kelley, S. P., Inger, S., Harris, N., & Okay, Aİ. (1999). 40Ar-39Ar and Rb-Sr geochronology of high-pressure metamorphism and exhumation history of the Tavşanlı Zone, NW Turkey. Contributions to Mineralgy and Petrology, 137, 46–58.
   Web of Science ®Google Scholar
• Shervais, J. W. (1982). Ti-V plots and the petrogenesis of modern ophiolitic lavas. Earth and Planetary Science Letters, 59, 101–118.10.1016/0012-821X(82)90120-0
   Web of Science ®Google Scholar
• Stern, R. J. (1979). On the origin of andesite in the northern Mariana Island arc: Implications from Agrigan. Contributions to Mineralogy and Petrology, 68, 207–219.10.1007/BF00371901
   Web of Science ®Google Scholar
• Stern, R. J., & Bloomer, S. H. (1992). Subduction zone infancy: Examples from the Eocene Izu-Bonin-Mariana and Jurassic California arcs. Geological Society of America Bulletin, 104, 1621–1636.10.1130/0016-7606(1992)104<1621:SZIEFT>2.3.CO;2
   Web of Science ®Google Scholar
• Sun, S. S., & McDonough, W. F. (1989). Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and proccesses. In A. D. Saunders, & M. J. Norry (Eds.), Magmatism in oceanic basins (Vol. 42, pp. 313–345). London: Geological Society, Special Publications.
   Google Scholar
• Thompson, G. (1991). Metamorphic and hydrothermal processes: Basalt-seawater interactions. In P. A. Floyd (Ed.), Oceanic basalts (pp. 148–173). Glasgow and London: Blackie.
   Google Scholar
• Topuz, G., Göçmengil, G., Rolland, Y., Çelik, Ö. F., Zack, T., & Schmitt, A. K. (2012). Jurassic accretionary and ophiolite from northeast Turkey: No evidence for the Cimmerian continental ribbon. Geology, 41, 255–258.
   Web of Science ®Google Scholar
• Uysal, İ., Ersoy, Y. E., Karslı, O., Dilek, Y., Sadıklar, M. B., Ottley, C. J., … Meisel, T. (2012). Coexistence of abyssal and ultra-depleted SSZ type mantle peridotites in a Neotethyan ophiolite in SW Turkey: Constraints from mineral composition, whole rock geochemistry (major-trace-REE-PGE), and Re-Os isotope systematics. Lithos, 132–133, 50–69.10.1016/j.lithos.2011.11.009
   Web of Science ®Google Scholar
• Vergili, Ö., & Parlak, O. (2005). Geochemistry and tectonic setting of metamorphic sole rocks and mafic dykes from the Pınarbaşı (Kayseri) ophiolite, Central Anatolia. Ofioliti, 30, 37–52.
   Web of Science ®Google Scholar
• Wallin, E. T., & Metcalf, R. V. (1998). Supra‐subduction zone ophiolite formed in an extensional forearc: Trinity Terrane, Klamath mountains, California. Journal of Geology, 106, 591–608.10.1086/516044
   Web of Science ®Google Scholar
• Whitney, D. L., & Dilek, Y. (1998). Metamorphism during Alpine crustal thickening and extension in Central Anatolia, Turkey: The Nigde metamorphic core complex. Journal of Petrology, 39, 1385–1403.10.1093/petroj/39.7.1385
   Web of Science ®Google Scholar
• Whitney, D. L., & Hamilton, M. A. (2004). Timing of high-grade metamorphism in central Turkey and the assembly of Anatolia. Journal of the Geological Society, 161, 823–828.10.1144/0016-764903-081
   Web of Science ®Google Scholar
• Whitney, D. L., Teyssier, C., Dilek, Y., & Fayon, A. K. (2001). Metamorphism of the central Anatolian Crystalline Complex, Turkey: İnfluence of orogen-normal collision vs. wrench-dominated tectonics on P-T-t paths. Journal of Metamorphic Geology, 19, 411–432.10.1046/j.0263-4929.2001.00319.x
   Web of Science ®Google Scholar
• Whitney, D. L., Teyssier, C., Fayon, A. K., Hamilton, M. A., & Heizler, M. (2003). Tectonic controls on metamorphism, partial melting, and intrusion: Timing and duration of regional metamorphism and magmatism in the Niğde Massif, Turkey. Tectonophysics, 376, 37–60.10.1016/j.tecto.2003.08.009
   Web of Science ®Google Scholar
• Winchester, J. A., & Floyd, P. A. (1977). Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology, 20, 325–343.10.1016/0009-2541(77)90057-2
   Web of Science ®Google Scholar
• Wood, D. A., Joron, J. L., & Treuil, M. (1979). A re-appraisal of the use of trace elements to classify and discriminate between magma series erupted in different tectonic settings. Earth and Planetary Science Letters, 45, 326–336.10.1016/0012-821X(79)90133-X
   Web of Science ®Google Scholar
• Yalınız, K. M., Floyd, P. A., & Göncüoğlu, M. C. (1996). Supra-subduction zone ophiolites of Central Anatolia: Geochemical evidence from the Sarikaraman ophiolite, Aksaray, Turkey. Mineralogical Magazine, 60, 697–710.
   Web of Science ®Google Scholar
• Yalınız, K. M., Floyd, P. A., & Göncüoğlu, M. C. (2000). Geochemistry of volcanic rocks from the Çiçekdağ Ophiolite, Central Anatolia, Turkey, and their inferred tectonic setting within the northern branch of the Neotethyan Ocean. In E. Bozkurt, J. A. Winchester, & J. D. A. Piper (Eds.), Tectonics and mangamism in Turkey and the surrounding area (Vol. 173, pp. 203–218). London: Geological Society, Special Publications.
   Google Scholar
• Yılmaz, H., Arıkal, T., & Yılmaz, A. (2001). Geology of the Güneş ophiolite (Divriği-Sivas). Proceedings of the 54th Geological Congress of Turkey, Ankara, pp. 54–65 (in Turkish with English Abstract).
   Google Scholar
• Yogodzinski, G. M., Volynets, O. N., Koloskov, A. V., Seliverstov, N. I., & Matvenkov, V. V. (1993). Magnesian andesites and the subduction component in strongly calc-alkaline series at Piip volcano, far western Aleutians. Journal of Petrology, 35, 163–204.
   Web of Science ®Google Scholar