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首页> 外文期刊>Geologia Croatica: a journal of the Institute of Geology Zagreb and Croatian Geological Society >Bio- and sequence stratigraphy of Upper Cretaceous - Palaeogene rocks, East Bahariya concession, Western Desert, Egypt
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Bio- and sequence stratigraphy of Upper Cretaceous - Palaeogene rocks, East Bahariya concession, Western Desert, Egypt

机译:上白垩统生物层序地层学-古近纪岩石,东巴哈里亚租界,埃及西部沙漠

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摘要

This work deals with the plankton stratigraphy of the subsurface Upper Cretaceous-Palaeogene succession of the East Bahariya Concession based on planktonic foraminifera and calcareous nannofossils. The examination of the cuttings from five wells: AQSA-1X, KARMA-E-1X, KARMA-3X, KARMA-NW-1X and KARMA-NW-5X is biostratigraphically evaluated. It is possible to identify the planktonic foraminifera as well as the calcareous nannofossil biozones. The analyses of calcareous nannofossils revealed the presence of several hiatuses. Information obtained from well data such as seismic facies analysis for the studied area has enabled classification of the Upper Cretaceous- Palaeogene succession into five major 2 nd order depositional sequences, separated by four major depositional sequence boundaries (SB1, SB2, SB3 and SB4). The Upper Cretaceous-Palaeogene succession in the East Bahariya is divided into 17 systems tracts. These systems tracts are: 7 System tracts of probable Cenomanian age, (the sequence stratigraphic framework as well as the cycles and system tracts of the Cenomanian Bahariya Formation match well with those of CATUNEANU et al., 2006); 4 System tracts of Turonian age, 2 System tracts of Campanian-Maastrichtian age and 4 System tracts of Eocene age.
机译:这项工作是基于浮游有孔虫和钙质纳米化石,对东巴哈里亚租界的地下白垩纪-古近纪演替的浮游生物地层进行研究。通过生物地层学评估了五个井中的钻屑检查:AQSA-1X,KARMA-E-1X,KARMA-3X,KARMA-NW-1X和KARMA-NW-5X。可以识别浮游有孔虫以及钙质纳米化石生物区。钙质纳米化石的分析揭示了几种裂隙的存在。从井眼数据中获得的信息(例如研究区域的地震相分析)已将上白垩统-古近纪演替划分为五个主要的二阶沉积层序,并由四个主要沉积层序边界(SB1,SB2,SB3和SB4)隔开。东巴哈里亚地区的上白垩统-古近纪演替被划分为17个系统带。这些系统域是:7可能为西诺曼纪年龄的系统域(层序地层框架以及西诺曼尼亚巴哈里亚组的旋回和系统域与CATUNEANU等人,2006)相匹配; Turonian时代的4个系统区域,Campanian-Maastrichtian时代的2个系统区域和始新世时代的4个系统区域。

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