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Late Cretaceous successive pelagic neptunian dike infillings within the middle-upper Cenomanian platform limestones of the eastern part of the Bey Dağları Carbonate Platform (Katran Dağ, Antalya, SW Turkey)

Year 2019, Volume: 40 Issue: 1, 35 - 71, 16.04.2019
https://doi.org/10.17824/yerbilimleri.501506

Abstract

Shallow marine Jurassic-Cretaceous carbonate succession is represented by abundant rudist bearing middle-late Cenomanian platform limestones (Yağca Köy Formation) at the top in the Katran Dağ area, which corresponds to the eastern part of the Bey Dağları Autochthon. Micritic pelagic neptunian dike infillings were first identified within the limestones accumulated in a platform edge environment in this study. Planktonic foraminifera and calcispheres observed in the infillings suggest a deeper marine conditions. These infillings were emplaced at least at three different times. The planktonic foraminiferal assemblages observed within the D2 and D3 infillings indicate that the infillings occurred during the late Coniacian-Santonian and latest Campanian Maastrichtian times. Although the D1 infilling predates the D2, the age can not be determined as the infilling does not have planktonic foraminifera. Likewise, the age of the infillings D4, D5 and D6 cutting the host rock of neritic limestones or D2 infilling can not be determined as well because of absence of planktonic foraminifera. Hovewer, facies characteristics of some parts of the infilling D4 are more or less similar to the infilling D3. Facies types and planktonic foraminiferal assemblages observed in the infillings D2 and D3 are similar to those documented in the widespread pelagic successions throughout the northern part of the Bey Dağları Autochthon. These data show that the onset and development of the pelagic deposition occurred in the eastern part of the platform as in the northern part. The pelagic deposits accumulated in the eastern part of the platform should have been eroded during the post Santonian and latest Maastrichtian erosional events. As the neptunian dike infillings are mostly associated with the platform drowning events as a result of extensional tectonics, the data obtained in this study suggest that this part of the platform was drowned during the late Coniacian-Santonian and latest Campanian-Maastrichtian as in the northern part of the platform. 

References

  • Anthonissen, D. E. ve Ogg, J. G., (derleyenler) (2012): Appendix 3: Cenozoic and Cretaceous biochronology of planktonic foraminifera and calcareous nannofossils. In: Gradstein, F. M., Ogg, J. G., Schmitz, M. D. ve Ogg, G.M. (eds.). The Geologic Time Scale 2012, Volume 2. Amsterdam, the Netherlands: Elsevier, pp. 1083-1127.
  • Bates R.L. ve Jackson J.A., 1987. Glossary of Geology, 3rd edn. American Geological Institute, Alexandria, Virginia, pp.335 ve 446.
  • Bektaş, O. ve Çapkınoğlu, Ş.,1997. Doğu Pontid magmatik arkında (KD Türkiye) neptüniyen dayklar ve blok tektoniği: Mesozoyik havzalarının kinematiği ile ilgili bulgular. Çukurova Univ. Jeoloji Eğitiminde 20 yıl sempozyomu, Bildiri Özetleri, 187-189, Adana.
  • Bektaş, O., Çapkınoğlu, Ş. ve Akdağ, K., 2001. Successive extensional tectonic regimes during the Mesozoic as evidenced by neptunian dikes in the Pontide Magmatic Arc, northeast Turkey. International Geology Review, 43, 840-849.
  • Bektaş, O., Çapkınoğlu, Ş. ve Akdağ, K., 2002. Neptüniyen dayklar ve tektonik önemleri. Mavi Gezegen, 5, 78-80.
  • Bignot, G. ve Poisson, A., 1974. Le Cénomanien du flanc oriental du Katran Dağ (Sam dağ) pres d’Antalya (Turquie). Bulletin of the Mineral Research and Exploration Institute of Turkey, 82, 71-77.
  • Blendinger, W., 1986. Isolated stationary carbonate platforms: the Middle Triassic (Ladinian) of the Marmolada area, Dolomites, Italy. Sedimentology, 33, 159-183.
  • Coccioni, R. ve Premoli Silva, I., 2015, Revised Upper Albian-Maastrichtian planktonic foraminiferal biostratigraphy and magnetostratigraphy of the classical Tethyan Gubbio section (Italy). Newsletter on Stratigraphy, 48(1), 47–90.
  • Cozzi, A., 2000. Synsedimentary tensional features in Upper- Triassic shallow-water carbonates of the Carnian Prealpes (northern Italy) and their importance as paleostress indicators. Basin Research, 12, 133-146.
  • Dercourt, J., Gaetani, M., Vrielynck, B., Barrier, E., Biju-Duval, B., Brunet, M. F., vd., (eds). 2000. Peri-Tethys Palaeogeographical Maps Atlas. Commission Carte Géologique du Monde-Commission Geological Map of the World. Paris.
  • Dunham, R. J., 1962. Classification of carbonate rocks according to depositional texture. In. W. E. Ham, (Ed). Classification of Carbonate Rocks. Am. Ass. Petrol. Geol. Mem. 1, 108-121.
  • Embry, A.F. ve Klovan, J.E., 1971. A Late Devonian reef tract on northeastern Banks Island, Northwest Territories. Can. Petrol. Geology Bull. 19, 730-781.
  • Farinacci, A. ve Köylüoğlu, M., 1982. Evolution of the Jurassic-Cretaceous Taurus Shelf (southern Turkey). Bolletino Della Societa Paleontologica Italiana 21, 267-276.
  • Farinacci, A., Yeniay, G., 1986. Biostratigraphy and event-analysis of the Cenomanian-Maastrichtian carbonates of the Bey Dağları (western Taurus, Turkey). Geologica Romana 25, 257-284.
  • Füchtbauer, H. ve Richter, D.K., 1983. Relations between submarine fissures, internal breccias and mass flow during Triassie and earlier rifting periods. Geologische Rundschau, 72 (1), 53-66.
  • Flügel, E., 2010. Microfacies of carbonate rocks. Analysis, interpretation and application. 2nd edition. Springer, Berlin, Heidelberg, New York, 984 p.
  • Gale, A.S., Kennedy, J.W., Lees, J.A., Petrizzo, M.R., Walaszczyk, I., 2007. An integrated study (inoceramid bivalves, ammonites, calcareous nannofossils, planktonic foraminifera, stable carbon isotopes) of the Ten Mile Creek section, Lancaster, Dallas County, north Texas, a candidate Global boundary Stratotype Section and Point for the base of the Santonian Stage. Acta Geologica Polonica, v. 57, pp. 113-160.
  • Göncüoğlu, M.C., 2011. Geology of the Kütahya-Bolkardağ Belt. M.T.A. Bulletin, 142, 223-277.
  • Gutnic, M., Monod, O., Poisson, A. ve Dumont, J.F., 1979. Géologie des Taurus occidentales (Turquie). Mémoires de la Société Géologique de France 58, 1-112.
  • Ion, J. ve Szasz, L., 1994. Biostratigraphy of the Upper Cretaceous of Romania. Cretaceous Research 15, 59-87.
  • Ion, J., Antonescu, E., Melinte, M. ve Szasz, L., 1999. Integrated biostratigraphy of the Lower and Middle Coniacian in Romania. Acta Palaeontologica Romaniae 2, 213-221.
  • Lamolda, M.A. ve Paul, C.R.C., 2007. Carbon and oxygen stable isotopes across the Coniacian/Santonian boundary at Olazagutia, northern Spain. Cretaceous Research 28 (1), 37-45.
  • Lehner, B.L., 1991. Neptunian dykes along a drowned Carbonate platform margin: an indication for recurrent extensional tectonic activity?. Terra Nova, 3, 593-606.
  • Ogg, J. G. ve Hinnov, L. A., 2012. Cretaceous. In: Gradstein, F. M., Ogg, J. G., Schmitz, M. D. ve Ogg, G.M. (eds.): The Geologic Time Scale 2012, Volume 2. Amsterdam, the Netherlands: Elsevier, pp. 793-854.
  • Okay, I.A. ve Tüysüz, O., 1999. Tethyan sutures of northern Turkey. Geological Society, London, Special Publications 156, 475-515.
  • Özgül, N., 1976. Some basic geological properties of Taurides. TJK Bülteni (Bulletin of Geological Society of Turkey) 19, 65-78.
  • Özgül, N., 1984. Stratigraphy and Tectonic evolution of the central Taurus. In: Tekeli, O., Göncüoğlu, M.C., (Eds.), Geology of the Taurus Belt, Proceedings, p. 77-90.
  • Özkan, S. ve Köylüoğlu, M., 1988. Campanian-Maastrichtian planktonic foraminiferal biostratigraphy of the Beydağları Autochtonous Unit, Western Taurids, Turkey. Middle East Technical University, Journal of Pure and Applied Sciences 21, 377-388.
  • Poisson, A., 1973. La coupe du Katran Dağ (Sam Dağ) pres d'Antalya (Taurus Lycien, Turquie). Decouverte de Jurassique et de Cretace inferieur. Mise en evidence d'une lacune dans le Cretace superieur. C.R. Acad. Sci. (d paraitre), Paris.
  • Poisson, A., 1977. Recherches géologiques dans les Taurides occidentals (Turquie). These Doct. d’Etat, Universitié de Paris-Sud, Orsay, 795 pp. (yayınlanmamış).
  • Poisson, A., Akay, E., Dumont, J.F. ve Uysal, Ş., 1984. The Isparta angle: a Mesozoic paleorift in the Western Taurides. In: Tekeli, O., Göncüoğlu, M.C. (Eds.), Geology of the Taurus Belt. International Symposium 26-29 September. 1983, Ankara 11-26.
  • Poisson, A., Yağmurlu, F., Bozcu, M. ve Şentürk, M., 2003. New insights on the tectonic setting and evolution of the Isparta Angle, SW Turkey. Geological Journal 38, 257-282.
  • Premoli Silva, I. ve Verga, D., 2004. Practical manual of Cretaceous planktonic foraminifera. In: Verga, D. ve Rettori, R. (eds.): International School on planktonic foraminifera, 3rd Course: Cretaceous. Universities of Perugia and Milan, Tiporafia Pontefelcino, Perugia (Italy), pp. 283.
  • Robaszynski, F., Gonzales Donoso, J. M., Linares, D., Amedro, F., Caron, M., Dupuis, C., Dhondt, A.V. ve Gartner, S., 2000. Le Crétacé supérieur de la région de Kalaat Senan, Tunisie centrale. Litho-biostratigraphie intégrée: zones d’ammonites, de foraminifères planctoniques et de nannofossiles du Turonien supérieur au Maastrichtien. Bulletin des Centres de Recherches Exploration-Production. Elf-Aquitaine 22, 359-490.
  • Robertson, A.H.F., Poisson, A. ve Akıncı, Ö., 2003. Developments in research concerning Mesozoic-Tertiary Tethys and neotectonics in the Isparta Angle, SW Turkey. Geological Journal, 38, 195-234.
  • Robertson, A.H.F., 1993. Mesozoic-Tertiary sedimentary and tectonic evolution of Neotethyan carbonate platforms, margins and small ocean basins in the Antalya Complex, southwest Turkey. International Assocciation of Sedimentologists, Special Publication, 20, 415-465
  • Sarı, B., 2006a. Upper Cretaceous planktonic foraminiferal biostratigraphy of the Bey Dağları autochthon in the Korkuteli Area, Western Taurides, Turkey. Journal of Foraminiferal Research 36, 241-261.
  • Sarı, B., 2006b. Foraminifera-rudist biostratigraphy, Sr-C-Isotope stratigraphy and microfacies analysis of the Upper Cretaceous sequences of the Bey Dağları autochthon (western Taurides, Turkey). PhD thesis, Dokuz Eylül University, İzmir, 436 pp. (yayınlanmamış).
  • Sarı, B., 2009. Planktonic foraminiferal biostratigraphy of the Coniacian-Maastrichtian sequences of the Bey Dağları Autochthon, western Taurides, Turkey: Thin section zonation. Cretaceous Research 30, 1103-1132.
  • Sarı, B. ve Özer, S., 2001. Facies characteristics of the Cenomanian-Maastrichtian sequence of the Beydağları carbonate platform in the Korkuteli area (western Taurides). International Geology Review 43, 830-839.
  • Sarı, B., ve Özer, S., 2002. Upper Cretaceous stratigraphy of the Beydağları carbonate platform, Korkuteli area (Western Taurides, Turkey). Turkish Journal of Earth Sciences, 11, 39-59.
  • Sarı, B., ve Özer, S., 2009. Upper Cretaceous rudist biostratigraphy of the Bey Dağları Carbonate Platform, Western Taurides, SW Turkey. Geobios, 42 (3), 359-380.
  • Sarı, B., Taslı, K. ve Özer, S., 2009. Benthonic foraminiferal biostratigraphy of the Upper Cretaceous (Middle Cenomanian-Coniacian) sequences of the Bey Dağları Carbonate Platform, western Taurides, Turkey. Turkish Journal of Earth Sciences, 18 (3), 393-425.
  • Schlische, R.W. ve Ackermann, R.V., 1995. Kinematic significance of sediment-filled fissures in the North Mountain Basalt, Fundy rift basin, Nova Scotia, Canada. Journal of Structural Geology, 17, 987-996.
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Bey Dağları Karbonat Platformu’nun doğu bölümünde orta-üst Senomaniyen platform kireçtaşlarında Geç Kretase yaşlı ardışık pelajik neptüniyen dayk dolguları (Katran Dağ, Antalya, GB Türkiye)

Year 2019, Volume: 40 Issue: 1, 35 - 71, 16.04.2019
https://doi.org/10.17824/yerbilimleri.501506

Abstract

Bey
Dağları Otoktonu’nun doğu bölümüne karşılık gelen Katran Dağ alanında sığ
denizel Jura-Kretase karbonat istifi en üstte orta-geç Senomaniyen yaşlı bol
rudistli platform kireçtaşları (Yağca Köy Formasyonu) ile temsil edilir.
Platform kenarı ortamında çökelmiş kireçtaşlarında daha derin ortamı işaret
eden planktonik foraminifer ve kalsisifer içeren en az üç farklı mikritik neptüniyen
dayk dolgusu tanımlanmıştır. D2 ve D3 dolgularında tanımlanan planktonik
foraminifer toplulukları, dolguların geç Koniasiyen-Santoniyen ve en geç
Kampaniyen-Maastrihtiyen’de gerçekleştiğini gösterir. D2 dolgusundan daha önce
gerçekleşen D1 dolgusunun yaşı planktonik foraminifer içermemesi nedeniyle
belirlenememektedir. Benzer şekilde, neritik kireçtaşları veya D2 dolgusundan
oluşan yan kayacı kesen D4, D5 ve D6 dolguları da karakteristik planktonik
foraminifer içermemeleri nedeniyle yaşlandırılamamaktadır. Ancak, özellikle D4
dolgusunun bazı bölümlerinin fasiyes özellikleri D3 dolgusu ile az çok
benzerdir. D2 ve D3 dolgularında tanımlanan fasiyes ve planktonik foraminifer
toplulukları Bey Dağları Otoktonu’nun kuzey bölümünde yaygın yüzlekleri bulunan
pelajik istifler ile oldukça benzerdir. Bu veri platformun kuzey bölümünde gözlenen
pelajikleşmenin platformun doğu bölümünde de gerçekleştiğini gösterir.
Platformun doğu bölümünde, Santoniyen sonrası ve Maastrihtiyen sonunda
gerçekleşen aşınma dönemlerinde pelajik istifler aşınmış olmalıdır. Neptüniyen
dayk dolguları çoğunlukla genleşme tektoniğine bağlı olarak gelişen platform
boğulmaları ile ilişkili olmaları nedeniyle, platformun bu bölümünün de kuzey
bölümde olduğu gibi geç Koniasiyen-Santoniyen ve en geç
Kampaniyen-Maastrihtiyen’de boğulduğunu gösterir.

References

  • Anthonissen, D. E. ve Ogg, J. G., (derleyenler) (2012): Appendix 3: Cenozoic and Cretaceous biochronology of planktonic foraminifera and calcareous nannofossils. In: Gradstein, F. M., Ogg, J. G., Schmitz, M. D. ve Ogg, G.M. (eds.). The Geologic Time Scale 2012, Volume 2. Amsterdam, the Netherlands: Elsevier, pp. 1083-1127.
  • Bates R.L. ve Jackson J.A., 1987. Glossary of Geology, 3rd edn. American Geological Institute, Alexandria, Virginia, pp.335 ve 446.
  • Bektaş, O. ve Çapkınoğlu, Ş.,1997. Doğu Pontid magmatik arkında (KD Türkiye) neptüniyen dayklar ve blok tektoniği: Mesozoyik havzalarının kinematiği ile ilgili bulgular. Çukurova Univ. Jeoloji Eğitiminde 20 yıl sempozyomu, Bildiri Özetleri, 187-189, Adana.
  • Bektaş, O., Çapkınoğlu, Ş. ve Akdağ, K., 2001. Successive extensional tectonic regimes during the Mesozoic as evidenced by neptunian dikes in the Pontide Magmatic Arc, northeast Turkey. International Geology Review, 43, 840-849.
  • Bektaş, O., Çapkınoğlu, Ş. ve Akdağ, K., 2002. Neptüniyen dayklar ve tektonik önemleri. Mavi Gezegen, 5, 78-80.
  • Bignot, G. ve Poisson, A., 1974. Le Cénomanien du flanc oriental du Katran Dağ (Sam dağ) pres d’Antalya (Turquie). Bulletin of the Mineral Research and Exploration Institute of Turkey, 82, 71-77.
  • Blendinger, W., 1986. Isolated stationary carbonate platforms: the Middle Triassic (Ladinian) of the Marmolada area, Dolomites, Italy. Sedimentology, 33, 159-183.
  • Coccioni, R. ve Premoli Silva, I., 2015, Revised Upper Albian-Maastrichtian planktonic foraminiferal biostratigraphy and magnetostratigraphy of the classical Tethyan Gubbio section (Italy). Newsletter on Stratigraphy, 48(1), 47–90.
  • Cozzi, A., 2000. Synsedimentary tensional features in Upper- Triassic shallow-water carbonates of the Carnian Prealpes (northern Italy) and their importance as paleostress indicators. Basin Research, 12, 133-146.
  • Dercourt, J., Gaetani, M., Vrielynck, B., Barrier, E., Biju-Duval, B., Brunet, M. F., vd., (eds). 2000. Peri-Tethys Palaeogeographical Maps Atlas. Commission Carte Géologique du Monde-Commission Geological Map of the World. Paris.
  • Dunham, R. J., 1962. Classification of carbonate rocks according to depositional texture. In. W. E. Ham, (Ed). Classification of Carbonate Rocks. Am. Ass. Petrol. Geol. Mem. 1, 108-121.
  • Embry, A.F. ve Klovan, J.E., 1971. A Late Devonian reef tract on northeastern Banks Island, Northwest Territories. Can. Petrol. Geology Bull. 19, 730-781.
  • Farinacci, A. ve Köylüoğlu, M., 1982. Evolution of the Jurassic-Cretaceous Taurus Shelf (southern Turkey). Bolletino Della Societa Paleontologica Italiana 21, 267-276.
  • Farinacci, A., Yeniay, G., 1986. Biostratigraphy and event-analysis of the Cenomanian-Maastrichtian carbonates of the Bey Dağları (western Taurus, Turkey). Geologica Romana 25, 257-284.
  • Füchtbauer, H. ve Richter, D.K., 1983. Relations between submarine fissures, internal breccias and mass flow during Triassie and earlier rifting periods. Geologische Rundschau, 72 (1), 53-66.
  • Flügel, E., 2010. Microfacies of carbonate rocks. Analysis, interpretation and application. 2nd edition. Springer, Berlin, Heidelberg, New York, 984 p.
  • Gale, A.S., Kennedy, J.W., Lees, J.A., Petrizzo, M.R., Walaszczyk, I., 2007. An integrated study (inoceramid bivalves, ammonites, calcareous nannofossils, planktonic foraminifera, stable carbon isotopes) of the Ten Mile Creek section, Lancaster, Dallas County, north Texas, a candidate Global boundary Stratotype Section and Point for the base of the Santonian Stage. Acta Geologica Polonica, v. 57, pp. 113-160.
  • Göncüoğlu, M.C., 2011. Geology of the Kütahya-Bolkardağ Belt. M.T.A. Bulletin, 142, 223-277.
  • Gutnic, M., Monod, O., Poisson, A. ve Dumont, J.F., 1979. Géologie des Taurus occidentales (Turquie). Mémoires de la Société Géologique de France 58, 1-112.
  • Ion, J. ve Szasz, L., 1994. Biostratigraphy of the Upper Cretaceous of Romania. Cretaceous Research 15, 59-87.
  • Ion, J., Antonescu, E., Melinte, M. ve Szasz, L., 1999. Integrated biostratigraphy of the Lower and Middle Coniacian in Romania. Acta Palaeontologica Romaniae 2, 213-221.
  • Lamolda, M.A. ve Paul, C.R.C., 2007. Carbon and oxygen stable isotopes across the Coniacian/Santonian boundary at Olazagutia, northern Spain. Cretaceous Research 28 (1), 37-45.
  • Lehner, B.L., 1991. Neptunian dykes along a drowned Carbonate platform margin: an indication for recurrent extensional tectonic activity?. Terra Nova, 3, 593-606.
  • Ogg, J. G. ve Hinnov, L. A., 2012. Cretaceous. In: Gradstein, F. M., Ogg, J. G., Schmitz, M. D. ve Ogg, G.M. (eds.): The Geologic Time Scale 2012, Volume 2. Amsterdam, the Netherlands: Elsevier, pp. 793-854.
  • Okay, I.A. ve Tüysüz, O., 1999. Tethyan sutures of northern Turkey. Geological Society, London, Special Publications 156, 475-515.
  • Özgül, N., 1976. Some basic geological properties of Taurides. TJK Bülteni (Bulletin of Geological Society of Turkey) 19, 65-78.
  • Özgül, N., 1984. Stratigraphy and Tectonic evolution of the central Taurus. In: Tekeli, O., Göncüoğlu, M.C., (Eds.), Geology of the Taurus Belt, Proceedings, p. 77-90.
  • Özkan, S. ve Köylüoğlu, M., 1988. Campanian-Maastrichtian planktonic foraminiferal biostratigraphy of the Beydağları Autochtonous Unit, Western Taurids, Turkey. Middle East Technical University, Journal of Pure and Applied Sciences 21, 377-388.
  • Poisson, A., 1973. La coupe du Katran Dağ (Sam Dağ) pres d'Antalya (Taurus Lycien, Turquie). Decouverte de Jurassique et de Cretace inferieur. Mise en evidence d'une lacune dans le Cretace superieur. C.R. Acad. Sci. (d paraitre), Paris.
  • Poisson, A., 1977. Recherches géologiques dans les Taurides occidentals (Turquie). These Doct. d’Etat, Universitié de Paris-Sud, Orsay, 795 pp. (yayınlanmamış).
  • Poisson, A., Akay, E., Dumont, J.F. ve Uysal, Ş., 1984. The Isparta angle: a Mesozoic paleorift in the Western Taurides. In: Tekeli, O., Göncüoğlu, M.C. (Eds.), Geology of the Taurus Belt. International Symposium 26-29 September. 1983, Ankara 11-26.
  • Poisson, A., Yağmurlu, F., Bozcu, M. ve Şentürk, M., 2003. New insights on the tectonic setting and evolution of the Isparta Angle, SW Turkey. Geological Journal 38, 257-282.
  • Premoli Silva, I. ve Verga, D., 2004. Practical manual of Cretaceous planktonic foraminifera. In: Verga, D. ve Rettori, R. (eds.): International School on planktonic foraminifera, 3rd Course: Cretaceous. Universities of Perugia and Milan, Tiporafia Pontefelcino, Perugia (Italy), pp. 283.
  • Robaszynski, F., Gonzales Donoso, J. M., Linares, D., Amedro, F., Caron, M., Dupuis, C., Dhondt, A.V. ve Gartner, S., 2000. Le Crétacé supérieur de la région de Kalaat Senan, Tunisie centrale. Litho-biostratigraphie intégrée: zones d’ammonites, de foraminifères planctoniques et de nannofossiles du Turonien supérieur au Maastrichtien. Bulletin des Centres de Recherches Exploration-Production. Elf-Aquitaine 22, 359-490.
  • Robertson, A.H.F., Poisson, A. ve Akıncı, Ö., 2003. Developments in research concerning Mesozoic-Tertiary Tethys and neotectonics in the Isparta Angle, SW Turkey. Geological Journal, 38, 195-234.
  • Robertson, A.H.F., 1993. Mesozoic-Tertiary sedimentary and tectonic evolution of Neotethyan carbonate platforms, margins and small ocean basins in the Antalya Complex, southwest Turkey. International Assocciation of Sedimentologists, Special Publication, 20, 415-465
  • Sarı, B., 2006a. Upper Cretaceous planktonic foraminiferal biostratigraphy of the Bey Dağları autochthon in the Korkuteli Area, Western Taurides, Turkey. Journal of Foraminiferal Research 36, 241-261.
  • Sarı, B., 2006b. Foraminifera-rudist biostratigraphy, Sr-C-Isotope stratigraphy and microfacies analysis of the Upper Cretaceous sequences of the Bey Dağları autochthon (western Taurides, Turkey). PhD thesis, Dokuz Eylül University, İzmir, 436 pp. (yayınlanmamış).
  • Sarı, B., 2009. Planktonic foraminiferal biostratigraphy of the Coniacian-Maastrichtian sequences of the Bey Dağları Autochthon, western Taurides, Turkey: Thin section zonation. Cretaceous Research 30, 1103-1132.
  • Sarı, B. ve Özer, S., 2001. Facies characteristics of the Cenomanian-Maastrichtian sequence of the Beydağları carbonate platform in the Korkuteli area (western Taurides). International Geology Review 43, 830-839.
  • Sarı, B., ve Özer, S., 2002. Upper Cretaceous stratigraphy of the Beydağları carbonate platform, Korkuteli area (Western Taurides, Turkey). Turkish Journal of Earth Sciences, 11, 39-59.
  • Sarı, B., ve Özer, S., 2009. Upper Cretaceous rudist biostratigraphy of the Bey Dağları Carbonate Platform, Western Taurides, SW Turkey. Geobios, 42 (3), 359-380.
  • Sarı, B., Taslı, K. ve Özer, S., 2009. Benthonic foraminiferal biostratigraphy of the Upper Cretaceous (Middle Cenomanian-Coniacian) sequences of the Bey Dağları Carbonate Platform, western Taurides, Turkey. Turkish Journal of Earth Sciences, 18 (3), 393-425.
  • Schlische, R.W. ve Ackermann, R.V., 1995. Kinematic significance of sediment-filled fissures in the North Mountain Basalt, Fundy rift basin, Nova Scotia, Canada. Journal of Structural Geology, 17, 987-996.
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There are 50 citations in total.

Details

Primary Language Turkish
Subjects Engineering
Journal Section Articles
Authors

Bilal Sarı 0000-0002-2389-2772

Publication Date April 16, 2019
Submission Date December 24, 2018
Acceptance Date April 5, 2019
Published in Issue Year 2019 Volume: 40 Issue: 1

Cite

EndNote Sarı B (April 1, 2019) Bey Dağları Karbonat Platformu’nun doğu bölümünde orta-üst Senomaniyen platform kireçtaşlarında Geç Kretase yaşlı ardışık pelajik neptüniyen dayk dolguları (Katran Dağ, Antalya, GB Türkiye). Yerbilimleri 40 1 35–71.