Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.oregeorev.2016.03.022 |
Transpressional imbricate thrust zones controlling gold mineralization in the Central Eastern Desert of Egypt | |
Abd El-Wahed, Mohamed A.1; Harraz, Hassan1; El-Behairy, Mohamed H.2 | |
通讯作者 | Abd El-Wahed, Mohamed A. |
来源期刊 | ORE GEOLOGY REVIEWS
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ISSN | 0169-1368 |
EISSN | 1872-7360 |
出版年 | 2016 |
卷号 | 78页码:424-446 |
英文摘要 | Strongly deformed volcaniclastic metasediments and ophiolitic slices hosting the Sukari gold mineralization display evidence of a complex structural evolution involving three main ductile deformational events (D-1-D-3). D1 produced ENE-trending folds associated with NNW-propagating thrust slices and intrusion of the Sukari granite (689 +/- 3 Ma). D-2 formed a moderately to steeply dipping, NNW-trending S-2 foliation curved to NE and developed arcuate structure constituting the Kurdeman shear zone (<= 595 Ma) and East Sukari imbricate thrust belt Major NE-trending F-2 folds, NW-dipping high-angle thrusts, shallow and steeply plunging mineral lineation and shear indicators recorded both subhorizontal and subvertical transport direction during D-2, D-3 (560-540 Ma) formed NNE-trending S-3 crenulation cleavage, tight F-3 folds, Sukari Thrust and West Sukari imbricate thrust The system of NW-trending sinistral Kurdeman shear zone (lateral ramps and tear faults) and imbricate thrusts (frontal ramps) forming the actuate structure developed during SE-directed thrusting, whereas the prevailing pattern of NNE-trending dextral Sukari shear zone and imbricate thrusts forming Sukari thrust duplex developed during NE-directed tectonic shearing. Sukari granite intruded in different pluses between 689 and 540 Ma and associated with at least four phases of quartz veins with different geometry and orientation. Structural analysis of the shear fabrics indicates that the geometry of the mineralized quartz veins and alteration patterns are controlled by the regional NNW- and NE-trending conjugate zones of transpression. Gold-bearing quartz veins are located within NNW-oriented sinistral shear zones in Kurdeman gold mine area, within steeply dipping NW- and SE dipping thrusts and NE- and NS-oriented dextral and sinistral shear zones around Sukari mine area, and along E-dipping backthrusts and NW-SE and N-S fractures in Sukari granite. The high grade of gold mineralization in Sukari is mainly controlled by SE-dipping back-thrusts branched from the major NW-dipping Sukari Thrust. The gold mineralization in Sukari gold mine and neighboring areas in the Central Eastern Desert of Egypt is mainly controlled by the conjugate shear zones of the Najd Fault System and related to E-W directed shortening associated with oblique convergence between East and West Gondwana. (C) 2016 Elsevier B.V. All rights reserved. |
英文关键词 | Transpression Sukari gold mine area Central Eastern Desert Imbricate thrust Thrust duplex |
类型 | Article |
语种 | 英语 |
国家 | Egypt |
收录类别 | SCI-E |
WOS记录号 | WOS:000378450300027 |
WOS关键词 | ARABIAN-NUBIAN SHIELD ; SHEAR ZONE ; STRUCTURAL EVOLUTION ; FLUID INCLUSION ; AFRICAN OROGEN ; CORE COMPLEX ; MINE ; AREA ; COLLISION ; GEOMETRY |
WOS类目 | Geology ; Mineralogy ; Mining & Mineral Processing |
WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/195269 |
作者单位 | 1.Tanta Univ, Dept Geol, Fac Sci, Tanta 31527, Egypt; 2.Centamin Egypt Ltd, 361 El Horreya Rd, Alexandria, Egypt |
推荐引用方式 GB/T 7714 | Abd El-Wahed, Mohamed A.,Harraz, Hassan,El-Behairy, Mohamed H.. Transpressional imbricate thrust zones controlling gold mineralization in the Central Eastern Desert of Egypt[J],2016,78:424-446. |
APA | Abd El-Wahed, Mohamed A.,Harraz, Hassan,&El-Behairy, Mohamed H..(2016).Transpressional imbricate thrust zones controlling gold mineralization in the Central Eastern Desert of Egypt.ORE GEOLOGY REVIEWS,78,424-446. |
MLA | Abd El-Wahed, Mohamed A.,et al."Transpressional imbricate thrust zones controlling gold mineralization in the Central Eastern Desert of Egypt".ORE GEOLOGY REVIEWS 78(2016):424-446. |
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