標(biāo)題: Titlebook: Ediacaran-Paleozoic Rock Units of Egypt; Their Correlation wi Mohamed Abdel Ghany Khalifa Book 2023 The Editor(s) (if applicable) and The A [打印本頁] 作者: Malevolent 時(shí)間: 2025-3-21 19:39
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書目名稱Ediacaran-Paleozoic Rock Units of Egypt影響因子(影響力)學(xué)科排名
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書目名稱Ediacaran-Paleozoic Rock Units of Egypt網(wǎng)絡(luò)公開度學(xué)科排名
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書目名稱Ediacaran-Paleozoic Rock Units of Egypt讀者反饋
書目名稱Ediacaran-Paleozoic Rock Units of Egypt讀者反饋學(xué)科排名
作者: 審問 時(shí)間: 2025-3-21 22:13 作者: GULLY 時(shí)間: 2025-3-22 02:17
https://doi.org/10.1007/978-3-031-27320-9Egypt, Jordon, Iraq and Saudi Arabia; Rock units; Ediacaran-Paleozoic; Correlation; Depositional environ作者: Inferior 時(shí)間: 2025-3-22 07:09
978-3-031-27322-3The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl作者: 思考 時(shí)間: 2025-3-22 10:52
ication, which includes the Hammamat and El Urf formations in the Easter Desert and Sinai. Furthermore, it provides geologic information about the Nubia Sandstone and its division into various rock units in the Western Desert. It connects Paleozoic rocks from the Western and Eastern Deserts, as well作者: ENNUI 時(shí)間: 2025-3-22 15:10
mmamat and the El Urf formations) belong to the Ediacaran Neoproterozoic, while the third (Abu Haswa Formation) belong to the Ediacaran sedimentary rocks. The Hammamat Formation refers to the Ediacaran clastic rocks found in an isolated basin within the Neoproterozoic rocks of Egypt’s central Easter作者: ENNUI 時(shí)間: 2025-3-22 18:39 作者: Pseudoephedrine 時(shí)間: 2025-3-22 23:27 作者: 悶熱 時(shí)間: 2025-3-23 04:04 作者: Original 時(shí)間: 2025-3-23 07:33 作者: 擁擠前 時(shí)間: 2025-3-23 12:34 作者: 催眠藥 時(shí)間: 2025-3-23 14:27 作者: 生命 時(shí)間: 2025-3-23 18:04
Ediacaran-Paleozoic Rock Units of Egypt978-3-031-27320-9Series ISSN 2730-6674 Series E-ISSN 2730-6682 作者: 灌溉 時(shí)間: 2025-3-24 01:04
2730-6674 leozoic rock units‘ description.Provides correlation of Edia.This book presents the following geological contributions in Ediacaran and Paleozoic rocks.?1) It introduces?four new rock units for the first time, the Ediacaran El Urf Formation (volcanoclastic?sediments in the central Eastern Desert), t作者: 競(jìng)選運(yùn)動(dòng) 時(shí)間: 2025-3-24 05:12 作者: Foam-Cells 時(shí)間: 2025-3-24 07:48 作者: 群島 時(shí)間: 2025-3-24 12:55 作者: Freeze 時(shí)間: 2025-3-24 18:52
Introduction and Back Ground History,ia Sandstone and its division into various rock units in the Western Desert. It connects Paleozoic rocks from the Western and Eastern Deserts, as well as the Sinai Peninsula. It depicts the distribution of Ediacaran and Paleozoic rocks on the surface and in the subsurface.作者: AMOR 時(shí)間: 2025-3-24 20:32
tween the basement rocks below and the Cambrian Araba Formation above. The lithofacies that make up the rock units mentioned above are described, and their depositional environments are interpreted. These rock units are correlated to neighbouring countries such as Libya, Jordan, and Saudi Arabia.作者: 眼界 時(shí)間: 2025-3-24 23:11 作者: 真繁榮 時(shí)間: 2025-3-25 07:18 作者: EXUDE 時(shí)間: 2025-3-25 10:04
End-Use Energy Consumption & CO2 Emissions,ormations in the Western Desert. A paleogeographic map is used to discuss their depositional environments. The abovementioned rock units will be correlated with equivalent rock units in Libya, Jordan, Saudi Arabia, and Iraq.作者: 淺灘 時(shí)間: 2025-3-25 15:43 作者: 冥想后 時(shí)間: 2025-3-25 19:15 作者: GOUGE 時(shí)間: 2025-3-25 22:07
The Silurian Period,iltstone and conglomerate beds. They range in age from the Early Silurian to the Late Silurian. These rocks are linked to their counterparts in Libya, Jordan, Saudi Arabia, and Iraq. A paleo-environmental map is created to depict the various depositional environments.作者: happiness 時(shí)間: 2025-3-26 02:05
The Carboniferous Period,ormations in the Western Desert. A paleogeographic map is used to discuss their depositional environments. The abovementioned rock units will be correlated with equivalent rock units in Libya, Jordan, Saudi Arabia, and Iraq.作者: Arable 時(shí)間: 2025-3-26 05:32
Book 2023the Ediacaran El Urf Formation (volcanoclastic?sediments in the central Eastern Desert), the Ediacaran Abu Haswa Formation (stromatolitic dolostone in southwestern Sinai), the Early Permian Wadi Dome Formation (mixed clastics and carbonates in the west of Suez Gulf) and the Early Permian Misawag?For作者: 怒目而視 時(shí)間: 2025-3-26 08:37
Book 2023sible depositional environments of the Ediacaran andPaleozoic rock units..Additionally, it offers an important unique geological information about the Ediacaran and Paleozoic rock units in Egypt. It unifies the nomenclature of Paleozoic rock units that take numerous names for the same geological tim作者: 有特色 時(shí)間: 2025-3-26 15:58
The Cambrian Period,alents rock units in Libya, Jordan, Saudi Arabia and Iraq. A paleogeographic map has been drawn all over the studied countries to manifest the facies changes and the possible depositional environment.作者: ARK 時(shí)間: 2025-3-26 17:10 作者: llibretto 時(shí)間: 2025-3-26 23:51 作者: NAUT 時(shí)間: 2025-3-27 01:20
alents rock units in Libya, Jordan, Saudi Arabia and Iraq. A paleogeographic map has been drawn all over the studied countries to manifest the facies changes and the possible depositional environment.作者: 披肩 時(shí)間: 2025-3-27 05:40
positional environments of the Permian rock units. The depositional environments of Egyptian rock units and their equivalent rock units in adjacent countries are interpreted using lithological types and faunal and floral associations.作者: Vaginismus 時(shí)間: 2025-3-27 11:05 作者: Conspiracy 時(shí)間: 2025-3-27 17:24
The Ediacaran Rock Units,mmamat and the El Urf formations) belong to the Ediacaran Neoproterozoic, while the third (Abu Haswa Formation) belong to the Ediacaran sedimentary rocks. The Hammamat Formation refers to the Ediacaran clastic rocks found in an isolated basin within the Neoproterozoic rocks of Egypt’s central Easter作者: 卷發(fā) 時(shí)間: 2025-3-27 21:04
The Cambrian Period,ora, palaeogeography, and tectonic events that occurred during this period. It describes two rock units in Egypt: the Middle Cambrian Araba Formation, which is visible on the surface, and the Shifa Formation, which is found in the subsurface at the Siwa basin in the northwestern Desert. This chapter作者: GREEN 時(shí)間: 2025-3-28 01:59 作者: 拍翅 時(shí)間: 2025-3-28 02:52
The Silurian Period, which are found in the subsurface in the Siwa basin in the northwestern Desert. The Um Ras formation is found in the Um Ras Plateau, northeast of Gebel Uweinat. It comprises a non-cyclic sequence of pale reddish massive sandstone with thin intercalations of horizontally bedded sandstone enriched wi作者: 谷類 時(shí)間: 2025-3-28 08:30 作者: 泰然自若 時(shí)間: 2025-3-28 12:40
The Carboniferous Period,l and floral associations, and other information. It is concerned with the Carboniferous rock units of Egypt and neighbouring countries. Lower Carboniferous rock units include the Umm Bogma and Abu Thora formations in southwest Sinai and the Wadi Malik Formation in the Gilf plateau in the southweste作者: dermatomyositis 時(shí)間: 2025-3-28 17:46
