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首页> 外文期刊>Cretaceous Research >First evidence of Campanian radiolarians in Turkey and implications for the tectonic setting of the Upper Antalya Nappes
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First evidence of Campanian radiolarians in Turkey and implications for the tectonic setting of the Upper Antalya Nappes

机译:土耳其Campanian放射虫的初步证据及其对安塔利亚上游尿布构造环境的影响

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The definition and inventory of the upper units of the Antalya Nappes or "Calcareous Antalya Nappes" (CAN) are still a matter of controversies and often conflicting interpretations. In the Gedeller type locality, we logged a new succession that sheds light on the detailed stratigraphy of the Upper Antalya Nappes. The lower part of the series corresponds to the uppermost part of the Kemer Gorge Nappe and is overthrust by the Ordovician Seydisehir Formation of the Tahtali Dag Nappe. The newly described Gedeller Formation belongs to the Kemer Gorge Nappe and is represented by Campanian (Upper Cretaceous) Scaglia-type pelagic limestones, which yielded radiolarians of the Amphipyndax pseudoconulus Zone. It is demonstrated that the "Calcareous Antalya Nappes" are composed of three different nappes, the Kemer Gorge, Bakirli and the Tahtali Dag nappes, all of them belonging to the Upper Antalya Nappes system.
机译:Antalya尿布或“ Calcareous Antalya尿布”(CAN)的上部单元的定义和清单仍然是一个有争议的问题,并且常常是相互矛盾的解释。在Gedeller型地区,我们记录了一个新的演替,以阐明上安塔利亚纳皮斯的详细地层学。该系列的下部对应于凯梅尔峡谷纳普河的最上部,并被塔塔利达格纳普河的奥陶纪塞西谢谢希尔组推覆。新近描述的吉德勒组属于凯梅尔峡谷纳佩,以坎帕尼(上白垩统)斯卡利亚型上层石灰岩为代表,产生了伪phi蛇区的放射虫。结果表明,“钙质安塔利亚尿布”由三个不同的尿布组成:凯梅尔峡谷,巴基里和塔塔利达格尿布,它们都属于上安塔利亚尿布系统。

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