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Stratigraphy and Microfauna (Radiolarians and Foraminifera) of the Upper Cretaceous (Upper Santonian–Lower Campanian) Carbonate Deposits in the Area of Struganik Village, Western Serbia)
Stratigraphy and Geological Correlation ( IF 1.0 ) Pub Date : 2020-03-25 , DOI: 10.1134/s0869593820010037
L. G. Bragina , N. Yu. Bragin , L. F. Kopaevich , N. Djerić , N. Gerzina Spajić

Abstract

Radiolarians and planktonic foraminifera were studied from the group of sections of the Upper Cretaceous lithographic limestones in the Struganik Village region (Western Serbia). The deposits studied were formed in the local basin that was surrounded by a carbonate platform and was characterized by low-energy conditions of sedimentation. The deposits are represented by micritic limestones with intercalations of calcarenites and rudites. The section of Struganik limestones has a small stratigraphic interval covering the upper Santonian and lower Campanian and having a total thickness of 120–150 m. Radiolarian zones (Crucella robusta and Afens perapediensis) and foraminiferal zones (equivalent of Dicarinella asymetrica and Globotruncanita elevata) were traced here.


中文翻译:

塞尔维亚西部Struganik村地区上白垩统(上Santonian–Campanian上)碳酸盐矿床的地层学和微动物区系(放射线虫和有孔虫)

摘要

放射线虫和浮游有孔虫是从斯特鲁尼克尼克村地区(西塞尔维亚)上白垩纪石印石灰岩剖面的一组中研究的。所研究的沉积物形成于一个被碳酸盐台地包围的局部盆地,其特征在于低能的沉积条件。沉积物是由钙镁矿和红晶石插入的微晶石灰岩代表的。Struganik石灰岩断层的地层间距很小,覆盖了上Santonian和下Campanian,总厚度为120-150 m。在此找到了放射虫区(鲁氏小Cr和Apers perapediensis)和有孔虫区(相当于不育双歧杆菌和Globotruncanita elevata)。
更新日期:2020-03-25
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