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Wapiennik Breccia Member (Pieniny Klippen Belt, Poland) – revised stratigraphy and origin

机译:Wapiennik Breccia成员(波兰Pieniny Klippen地带)–修订的地层学和成因

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摘要

The Wapiennik Breccia Member was originally attributed to the Czorsztyn Limestone Formation of the Czorsztyn Succession in the Pieniny Klippen Basin. The breccia was assigned previously to the Callovian–Oxfordian. Based on micropalaeontological and microfacies studies we have determined its age as late Albian. At this time the Czorsztyn Swell was affected by extensional faulting, with subsequent submarine erosion of scarps. The re-evaluated age of the breccia, as well as the lithology of its clasts and its matrix that contains Cretaceous foraminifera, indicate the assignment of the Wapiennik Breccia Member to the Chmielowa Formation.
机译:Wapiennik Breccia成员最初归因于Pieniny Klippen盆地Czorsztyn演替的Czorsztyn灰岩地层。角砾岩以前被分配给卡洛夫阶-牛津阶。根据微古生物学和微相研究,我们确定了它的晚期阿尔比时代。这时Czorsztyn Swell受到伸展断裂的影响,随后海底陡坡侵蚀。角砾岩年龄的重新评估,以及其碎屑和包含白垩纪有孔虫的基质的岩性,表明Wapiennik Breccia成员已归属Chmielowa组。

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