Arid
DOI10.1016/j.jafrearsci.2022.104452
Evidence for Upper Cretaceous seismites in the Abu Tartur area, Western Desert, Egypt
Hassan, Walaa A.; Ahmed, Ezzat A.; Sawires, Rashad; Moneim, Mohamed A.; Abukhadra, Mostafa R.
通讯作者Sawires, R (corresponding author),Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt.
来源期刊JOURNAL OF AFRICAN EARTH SCIENCES
ISSN1464-343X
EISSN1879-1956
出版年2022
卷号187
英文摘要Upper Cretaceous tidal-flat sediments of the Abu Tartur region, Western Desert of Egypt, contain a variety of softsediment deformation structures (SSDSs) in the Mut Member of the Quseir Formation and the overlying Duwi Formation. Here, we document recognition of a set of SSDSs characterized by complex morphology and large size. The SSDS include: 1) water-escape structures, 2) minor recumbent, chevron, and slump folds, 3) synsedimentary minor faults, 4) neptunian dykes, 5) regular ball-and-pillow structures, flattened pseudo-nodules, and load casts, 6) syn-sedimentary undulations, 7) fractures and joints, 8) sand injectites, and 9) autoclastic breccia and brecciated siderite clasts. The dimensions of the SSDSs range from a few centimeters to several decimeters. Both extensional and contractional forces appear to have been involved in development of these structures. A detailed analysis of facies relationships, combined with consistent orientations of SSDSs and the regional tectonics of the target area suggests earthquakes as the triggering mechanism for sediment deformation and large-scale mass failure. The deformed strata are consistent with most of the well-known criteria of typical seismites. Thus, syn-sedimentary liquefaction was identified as the primary driving force in most of the observed deformation horizons for these Upper Cretaceous SSDSs in the Abu Tartur area.
英文关键词Soft-sediment deformation structures Upper cretaceous Seismites Quseir and Duwi formations Abu Tartur Egypt
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000745076200003
WOS关键词SOFT-SEDIMENT DEFORMATION ; SYNSEDIMENTARY DEFORMATION ; LACUSTRINE SEDIMENTS ; CONTINENTAL-MARGIN ; STRONG EARTHQUAKES ; PANCHET FORMATION ; LAKE-SEDIMENTS ; BASIN ; FAULT ; DEPOSITS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/376260
作者单位[Hassan, Walaa A.; Ahmed, Ezzat A.; Sawires, Rashad; Moneim, Mohamed A.] Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt; [Abukhadra, Mostafa R.] Beni Suef Univ, Fac Sci, Dept Geol, Mat Technol & Their Applicat Lab, Bani Suwayf, Egypt
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GB/T 7714
Hassan, Walaa A.,Ahmed, Ezzat A.,Sawires, Rashad,et al. Evidence for Upper Cretaceous seismites in the Abu Tartur area, Western Desert, Egypt[J],2022,187.
APA Hassan, Walaa A.,Ahmed, Ezzat A.,Sawires, Rashad,Moneim, Mohamed A.,&Abukhadra, Mostafa R..(2022).Evidence for Upper Cretaceous seismites in the Abu Tartur area, Western Desert, Egypt.JOURNAL OF AFRICAN EARTH SCIENCES,187.
MLA Hassan, Walaa A.,et al."Evidence for Upper Cretaceous seismites in the Abu Tartur area, Western Desert, Egypt".JOURNAL OF AFRICAN EARTH SCIENCES 187(2022).
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