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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Upper Jurassic-Lower Cretaceous depositional environments and evolution of the Bilecik (Sakarya Zone) and Tauride carbonate platforms, Turkey
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Upper Jurassic-Lower Cretaceous depositional environments and evolution of the Bilecik (Sakarya Zone) and Tauride carbonate platforms, Turkey

机译:土耳其上侏罗统-下白垩统沉积环境以及比勒奇克(萨卡里亚地区)和陶瑞德碳酸盐台地的演化

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摘要

Three Late Jurassic-Early Cretaceous carbonate platform stratigraphic sections have been studied in central western Turkey (Bilecik carbonate platform at Bilecik and Saricakaya) and in the Taurides in southern Turkey (Tauride carbonate platform at Beysehir) by using sedimentological and cyclostratigraphical methods. One section was analyzed by detailed magnetic susceptibility measurements. Peritidal carbonates on both platforms display cyclic patterns throughout the sections and do not contain any siliciclastic material. This cyclicity is generally expressed as shallowing upward cycles and interpreted as records of short-term sea-level changes.
机译:通过沉积学和旋回地层学方法,已经在土耳其中部西部(比利西克和萨里卡卡亚的比利奇克碳酸盐台地)和土耳其南部的陶里德(贝西希尔的陶瑞德碳酸盐台地)研究了三个侏罗纪-早白垩纪碳酸盐台地层剖面。通过详细的磁化率测量来分析一节。两个平台上的蠕状碳酸盐均在整个剖面上显示出循环模式,并且不含任何硅质碎屑物质。这种周期性通常表示为向上的浅化周期,并解释为短期海平面变化的记录。

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