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Titlebook: Sequence Stratigraphy of the Lower Miocene Moghra Formation in the Qattara Depression, North Western; Safiya M. Hassan Book 2013 The Edito

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發(fā)表于 2025-3-21 18:22:02 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Sequence Stratigraphy of the Lower Miocene Moghra Formation in the Qattara Depression, North Western
編輯Safiya M. Hassan
視頻videohttp://file.papertrans.cn/866/865369/865369.mp4
概述Numerous color photos from excellent outcrops in the Northwestern Desert of Egypt.New sedimentological model and high-resolution sequence stratigraphy for a hitherto understudied sequence in the Quatt
叢書名稱SpringerBriefs in Earth Sciences
圖書封面Titlebook: Sequence Stratigraphy of the Lower Miocene Moghra Formation in the Qattara Depression, North Western;  Safiya M. Hassan Book 2013 The Edito
描述The Qattara Depression is part of the Northwestern Desert in Egypt and is home to the second lowest point in Africa at -133 meters below sea level. Therefore, before any projects can be carried out in this area, we must first understand the geology of the land. The present study deals with the high-resolution sequence stratigraphic analysis of the Lower Miocene Moghra Formation outcrops in the Qattara Depression Region. The literature on the sedimentology and sequence stratigraphy of the Moghra Formation has been sparse to date, despite some excellent work over the years by academic and petroleum workers. Moreover, the area studied is within what was once a front-line of World War II, where mine fields and war relics are scattered and cover wide reaches. This has resulted in limited geologic mapping in the past. Thus, great attention is paid in this study to establishing a robust sedimentology and high-resolution sequence stratigraphic framework for the Lower Miocene Moghra Formation. Included are works based on outcrops and, most importantly, new sedimentological and chronostratigraphic information not previously available.
出版日期Book 2013
關(guān)鍵詞Aheimer Formation; Carboniferous-Permian; Gulf of Suez; Lower Miocene; Moghra Formation; Northwestern Des
版次1
doihttps://doi.org/10.1007/978-3-319-00330-6
isbn_softcover978-3-319-00329-0
isbn_ebook978-3-319-00330-6Series ISSN 2191-5369 Series E-ISSN 2191-5377
issn_series 2191-5369
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl
The information of publication is updating

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Sedimentary Facies,arsening upward deltaic deposits; and (8) Fining upward channel deposits. These eight lithofacies associations are grouped into three main depositional environments: (1) Transgressive tide-dominated estuaries, (2) Open Shelf and (3) Regressive tide-dominated deltas.
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Stratigraphy,nteen units according to lithology. The first unit is represented by marine fine-grained siliciclastic deposits with . trace fossils (Unit I), and this is overlain by Unit II that consists of shallow marine coarse-grained siliciclastic deposits. This unit is rich in vertebrate fossil fragments. Unit
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Conclusion,tes. Despite this successful focus on the vertebrate of Moghra area, there is still a noticeable gap in our knowledge about Lower Miocene sedimentology and sequence stratigraphy of this area. The literature about the sedimentology and petroleum geology of this part of the Moghra Formation has been s
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