Structural evolution of the southern transfer zone of the Gulf of Suez rift, Egypt
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- 作者：Ali M.A. Abd-Allaha ; aliabdallah62@hotmail.com" class="auth_mail ; Mohamed H. Abdel Aalb ; mabdelaal81@yahoo.com" class="auth_mail ; Mohamed M. El-Saidc ; Ahmed Abd El-Nabya ; zowail2000@yahoo.com" class="auth_mail
- 关键词：Transfer zone ; Faulted blocks ; Pre-existing fault reactivations ; Gulf of Suez rift ; Syrian Arc system ; Egypt
- 刊名：Journal of African Earth Sciences
- 出版年：August 2014
- 年：2014
- 卷：96
- 期：Complete
- 页码：21-38
- 全文大小：14791 K
文摘
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The reactivations of the Precambrian fractures controlled the southern transfer zone.
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Syrian arc contraction controlled the sedimentation and structures of the pre-rift rocks.
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Oligo-Miocene rifting inverted the fault slip and rotated the Cretaceous reverse faults.
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Positive flower structures and reverse faults are oriented obliquely to the transfer zone.