High-resolution sequence stratigraphic correlation in the Upper Jurassic (Kimmeridgian)-Upper Cretaceous (Cenomanian) peritidal carbonate deposits (Western Taurides, Turkey)

Date

1999-01-01

Author

Altıner, Demir
Yılmaz, İsmail Ömer
Bayazitoglu, M
Gaziulusoy, ZE

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Upper Jurassic (Kimmeridgian)- Upper Cretaceous (Cenomanian) inner platform carbonates in the Western Taurides are composed of metre-scale upward-shallowing cyclic deposits (parasequences) and important karstic surfaces capping some of the cycles. Peritidal cycles (shallow subtidal facies capped by tidal-Aat laminites or fenestrate limestones) are regressive- and transgressive-prone (upward-deepening followed by upward-shallowing facies trends). Subtidal cycles are of two types and indicate incomplete shallowing. Submerged subtidal cycles are composed of deeper subtidal facies overlain by shallow subtidal facies. Exposed subtidal cycles consist of deeper subtidal facies overlain by shallow subtidal facies that are capped by features indicative of prolonged subaerial exposure. Subtidal facies occur characteristically in the Jurassic, while peritidal cycles are typical for the Lower Cretaceous of the region.

Subject Keywords

Western taurides, Biostratigraphy, Kimmeridgian-cenomanian, Peritidal carbonates, Metre-scale cycle, Sequence, Parasequence, Eustatic sea level, Orbital eccentricity cycle, Correlation

URI

https://hdl.handle.net/11511/55122

Journal

GEOLOGICAL JOURNAL

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Department of Geological Engineering, Article

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Citation Formats

D. Altıner, İ. Ö. Yılmaz, M. Bayazitoglu, and Z. Gaziulusoy, “High-resolution sequence stratigraphic correlation in the Upper Jurassic (Kimmeridgian)-Upper Cretaceous (Cenomanian) peritidal carbonate deposits (Western Taurides, Turkey),” GEOLOGICAL JOURNAL, pp. 139–158, 1999, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/55122.