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Ediacaran-paleozoic rock units of Egypt = their correlation with adjacent countries and their depositional environments /

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Ediacaran-paleozoic rock units of Egypt/ by Mohamed Abdel Ghany Khalifa.
其他題名:	their correlation with adjacent countries and their depositional environments /
作者:	Khalifa, Mohamed Abdel Ghany.
出版者:	Cham :Springer International Publishing : : 2023.,
面頁冊數:	xviii, 209 p. :ill., digital ; : 24 cm.;
Contained By:	Springer Nature eBook
標題:	Geodynamics. -
電子資源:	https://doi.org/10.1007/978-3-031-27320-9
ISBN:	9783031273209

Ediacaran-paleozoic rock units of Egypt = their correlation with adjacent countries and their depositional environments /
Khalifa, Mohamed Abdel Ghany.

Ediacaran-paleozoic rock units of Egypttheir correlation with adjacent countries and their depositional environments /[electronic resource] :by Mohamed Abdel Ghany Khalifa. - Cham :Springer International Publishing :2023. - xviii, 209 p. :ill., digital ;24 cm. - Earth and environmental sciences library,2730-6682. - Earth and environmental sciences library..

Chapter 1. Introduction and Back Ground History -- Chapter 2. The Ediacaran rock units -- Chapter 3. The Cambrian Period -- Chapter 4. The Ordovician Period -- Chapter 5. The Silurian Period -- Chapter 6. The Devonian Period -- Chapter 7. The Carboniferous Period -- Chapter 8. The Permian Period.

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), 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 Formation (in the subsurface, northwestern Desert), 2) making correlation of the Ediacaran rock units with the corresponding rock units in Libya, Jordan, Iraq and Saudi Arabia, 3) linking the exposed Paleozoic rock units with their equivalent rock units in subsurface in northwestern desert, 4) correlating the Paleozoic rock units with the equivalent rock units in adjacent countries, e. g. Libya, Jordan, Iraq and Saudi Arabia, 5) manifesting the possible depositional environments of the Ediacaran and Paleozoic 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 time. It obsoletes the formation names that do not follow the rules of the North American stratigraphic code (1983) for rock units' nomenclature. It provides the target audience illustrations, e.g. field photographs for the exposed rock units that save efforts and time for audience (undergraduate, post-graduate, researchers and professional) to reach to the original localities of each rock units. It provides the audience with schematic diagrams that exhibit the link between the exposed and subsurface rock units all over the Egyptian territory. It describes the following topics of each rock unit: definition, stratigraphic contact, lithological characteristics, faunal and floral associations that are used for the identification of the possible age, correlation with corresponding rock units in adjacent countries, e.g. Libya, Jordan, Iraq and Saudi Arabia and the possible depositional environments for each rock units. The book is a fundamental source of an updated version of the information in the field to the undergraduate, graduate, researchers, professional, practitioners and policy planning elsewhere.

ISBN: 9783031273209

Standard No.: 10.1007/978-3-031-27320-9doiSubjects--Topical Terms:

676804
Geodynamics.

LC Class. No.: QE653.5 / .K43 2023

Dewey Class. No.: 551.7150962

Ediacaran-paleozoic rock units of Egypt = their correlation with adjacent countries and their depositional environments /
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505 0 $a Chapter 1. Introduction and Back Ground History -- Chapter 2. The Ediacaran rock units -- Chapter 3. The Cambrian Period -- Chapter 4. The Ordovician Period -- Chapter 5. The Silurian Period -- Chapter 6. The Devonian Period -- Chapter 7. The Carboniferous Period -- Chapter 8. The Permian Period.
520 $a 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), 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 Formation (in the subsurface, northwestern Desert), 2) making correlation of the Ediacaran rock units with the corresponding rock units in Libya, Jordan, Iraq and Saudi Arabia, 3) linking the exposed Paleozoic rock units with their equivalent rock units in subsurface in northwestern desert, 4) correlating the Paleozoic rock units with the equivalent rock units in adjacent countries, e. g. Libya, Jordan, Iraq and Saudi Arabia, 5) manifesting the possible depositional environments of the Ediacaran and Paleozoic 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 time. It obsoletes the formation names that do not follow the rules of the North American stratigraphic code (1983) for rock units' nomenclature. It provides the target audience illustrations, e.g. field photographs for the exposed rock units that save efforts and time for audience (undergraduate, post-graduate, researchers and professional) to reach to the original localities of each rock units. It provides the audience with schematic diagrams that exhibit the link between the exposed and subsurface rock units all over the Egyptian territory. It describes the following topics of each rock unit: definition, stratigraphic contact, lithological characteristics, faunal and floral associations that are used for the identification of the possible age, correlation with corresponding rock units in adjacent countries, e.g. Libya, Jordan, Iraq and Saudi Arabia and the possible depositional environments for each rock units. The book is a fundamental source of an updated version of the information in the field to the undergraduate, graduate, researchers, professional, practitioners and policy planning elsewhere.
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