Arid
DOI10.1016/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
ISSN0169-1368
EISSN1872-7360
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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