Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.jseaes.2021.104782 |
Remote sensing and structural studies of the Central Asir Shear Zone, Western Arabian Shield: Implications for the late Neoproterozoic E-W Gondwana assembly | |
Hamimi, Zakaria; Abdelkareem, Mohamed; Fowler, Abdel-Rahman; Younis, Mohammed H.; Matsah, Mohammed; Abdalla, Fathy | |
通讯作者 | Abdelkareem, M ; Abdalla, F (corresponding author), South Valley Univ, Geol Dept, Qena 83523, Egypt. ; Abdalla, F (corresponding author), King Saud Univ, Geol & Geophys Dept, Chair Nat Hazards & Mineral Resources, Riyadh, Saudi Arabia. |
来源期刊 | JOURNAL OF ASIAN EARTH SCIENCES |
ISSN | 1367-9120 |
EISSN | 1878-5786 |
出版年 | 2021 |
卷号 | 215 |
英文摘要 | The Central Asir Shear Zone (CASZ) is a N- to NNE-oriented inhomogeneous strain zone parallel to the Nabitah shear belt in southern Saudi Arabia. It is -200 km long and 20 km wide, and traverses the Asir terrane. The deformed terrains in the vicinity of the CASZ have experienced a prolonged history involving three successive phases of deformation: arc-collision, dextral transpression and sinistral strike-slip faulting. Remote-sensing data analysis and field investigation provide insights into the geological and structural features along the CASZ. Image transformation and enhancement reveal faults and folds, and discriminate between granitoids, metavolcanics, gabbros and younger (Ablah Group) sediments. The obtained evidence points to polyphase deformation of the area, characterized by narrow zones of high strain, folding and shearing enclosing slices of less deformed rocks. Lineament analysis shows predominantly NNE, NNW, N and NE trends of folds and shear zones, and NW, NE and E fracture trends. The CASZ has a >100 m.y. long deformation history, including a change from dextral to sinistral shearing. Both shearing senses are found on the older N-S and younger NW-SE fault systems. N-S oriented shearing was accompanied by intrusion of granitoids and localized hydrothermal alteration along N to NNE trending shear zones. Strain analysis shows low strain in the Ablah basin sediments, consistent with Ablah deposition after the tectonic climax in the region. |
英文关键词 | Central Asir Shear Zone Structural analysis Arabian Shield Asir terrane East African Orogen |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000657697900001 |
WOS关键词 | CENTRAL EASTERN DESERT ; NAJD FAULT SYSTEM ; RED-SEA HILLS ; FINITE STRAIN ; STATISTICAL-ANALYSIS ; SAUDI-ARABIA ; EVOLUTION ; EXTRACTION ; EGYPT ; FIELD |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
来源机构 | King Saud University |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/350735 |
作者单位 | [Hamimi, Zakaria] Benha Univ, Fac Sci, Geol Dept, Banha 13518, Egypt; [Abdelkareem, Mohamed; Abdalla, Fathy] South Valley Univ, Geol Dept, Qena 83523, Egypt; [Fowler, Abdel-Rahman] United Arab Emirates Univ, Geol Dept, Al Ain, U Arab Emirates; [Younis, Mohammed H.] Aswan Univ, Geol Dept, Fac Sci, Aswan 81528, Egypt; [Matsah, Mohammed] King Abdulaziz Univ, Dept Struct Geol & Remote Sensing, Fac Earth Sci, Jeddah, Saudi Arabia; [Abdalla, Fathy] King Saud Univ, Geol & Geophys Dept, Chair Nat Hazards & Mineral Resources, Riyadh, Saudi Arabia |
推荐引用方式 GB/T 7714 | Hamimi, Zakaria,Abdelkareem, Mohamed,Fowler, Abdel-Rahman,et al. Remote sensing and structural studies of the Central Asir Shear Zone, Western Arabian Shield: Implications for the late Neoproterozoic E-W Gondwana assembly[J]. King Saud University,2021,215. |
APA | Hamimi, Zakaria,Abdelkareem, Mohamed,Fowler, Abdel-Rahman,Younis, Mohammed H.,Matsah, Mohammed,&Abdalla, Fathy.(2021).Remote sensing and structural studies of the Central Asir Shear Zone, Western Arabian Shield: Implications for the late Neoproterozoic E-W Gondwana assembly.JOURNAL OF ASIAN EARTH SCIENCES,215. |
MLA | Hamimi, Zakaria,et al."Remote sensing and structural studies of the Central Asir Shear Zone, Western Arabian Shield: Implications for the late Neoproterozoic E-W Gondwana assembly".JOURNAL OF ASIAN EARTH SCIENCES 215(2021). |
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