Stratigraphy and Larger Foraminifera of the Eocene Shallow marine and Olistostromal Units of the Southern Part of the Thrace Basin NW Turkey

Date

2010-01-01

Author

Yılmaz, İsmail Ömer
Gyoergy, Less

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https://hdl.handle.net/11511/72323

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Turkish Journal of Earth Sciences

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Stratigraphy and Larger Foraminifera of the Eocene Shallow-marine and Olistostromal Units of the Southern Part of the Thrace Basin, NW Turkey Özcan, Ercan; Less, Gyoergy; Okay, Aral; Baldi-Beke, Maria; Kollanyi, Katalin; Yılmaz, İsmail Ömer (2010-01-01) The Eocene marine sequence in the southern part of the Thrace Basin (NW Turkey) involves a variety of platform and deep-marine olistostromal units, the stratigraphy of which have been vigorously debated in the past. A detailed analysis of larger foraminifera in these either foraminifera or foraminifera-coral-coralline algae-dominated platform and associated comparatively deeper-marine units permits us to establish a high-resolution biostratigraphy in the context of shallow benthic zonation (with SBZ zones) ...
Stratigraphy and pre-Miocene tectonic evolution of the southwestern part of the Sivas Basin, Central Anatolia, Turkey Dirik, K; Göncüoğlu, Mehmet Cemal; Kozlu, H (1999-07-01) In central Anatolia there are several important basins developed mainly after closure of the northern branch of Neotethys. These are the Haymana, Tuzgolu, Ulukisla, Kizihrmak, Cankiri-Corum and Sivas basins. The Sivas Basin is located in the eastern part of central Anatolia between the Central Anatolian Crystalline Complex (CACC) in the north and Taurides in the south. The basement to the southeastern part of the basin consists of recrystallized limestone and clastics of the Permian-Lower Cretaceous Bunyan ...
Stratigraphy of megablocks within the "anatolian ophiolitic melange" around Balıkkuyumcu, southwest Ankara, Turkey. Çetintaş, Hülya; Department of Geological Engineering (1985)
Stratigraphic and micropaleontologic investigation of the Alakır-ı well (Finike), western taurids, Turkey Özcan, Ercan; Altıner, Demir; Department of Geological Engineering (1986)
Stratigraphic transition and palaeoenvironmental changes from the Aptian oceanic anoxic event 1a (OAE1a) to the oceanic red bed 1 (ORB1) in the Yenicesihlar section, central Turkey Hu, Xiumian; Zhao, Kuidong; Yılmaz, İsmail Ömer; Li, Yongxiang (2012-12-01) We performed a detailed study of the stratigraphic transition from the early Aptian oceanic anoxic event 1a (OAE1a) to the oceanic red bed 1 (ORB1) along the pelagic Yenicesihlar section in the Mudurnu region of central Turkey. The Selli-equivalent level of the OAE1a (approximately 2.1 m thick) consists of black to dark-grey shales interbedded with grey marlstones with total organic carbon contents up to 2.05%. The carbon isotopic record shows a negative excursion (C3 stage, 0.58 m in thick) at the bottom o...

Citation Formats

İ. Ö. Yılmaz and L. Gyoergy, “Stratigraphy and Larger Foraminifera of the Eocene Shallow marine and Olistostromal Units of the Southern Part of the Thrace Basin NW Turkey,” Turkish Journal of Earth Sciences, pp. 27–77, 2010, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/72323.