Geological studies and structural analysis of the Umm Anab metavolcanics and related quartz veins: implications for Pan-African volcanism in the Egyptian Nubian Shield

Khaled El-Gameel, Sara Fayed, H. El Desouky, Ashraf Abdelmaksoud
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Abstract

HE NEOPROTEROZOIC basement complex of the Umm Anab area is located 40 km southwest of Hurghada city in the Northern Eastern Desert (NED) of Egypt. The basement rocks include metavolcanics and enormous plutons of granitoid rocks. The metavolcanics are regionally metamorphosed, forming greenschist to amphibolite facies rocks interbedded with banded iron formation (BIF). Structural analysis in the Umm Anab metavolcanics (UAV) indicates that the area has a poly-phase structural deformation, and each phase has its own effect and style. A Well-developed schistosity striking approximately E-W with dipping 60º-80º southward, and asymmetrical folds with oblique subvertical NNW-striking axial planes were observed. The structural analysis of the veins in metavolcanic by using GArcmB software determined the paleostress inversion and displayed two clusters of veins that formed under two stresses. The stress ratios ( Φ )= ( σ 2 – σ 3) / ( σ 1 – σ 3) for both clusters, respectively, are ~0.39 and ~0.16, which shows two stress status. The values of the stress ratio on vein walls suggest that the host rock was subject to low to moderate tectonic stress at the time the veins formation. In addition, finite strain results in metavolcanics were estimated using the Rf/φ method on deformed pebbles (with a trend of N73º-88ºE), confirming the idea that metavolcanics are affected by low to moderate deformation. The stretching mineral lineation and BIF have trend ENE-WSW to E-W that supports the oldest shortening event (D1) which is considered an early phase of deformation NNW–SSE linked with the Pan-African thrusting.
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乌姆阿纳布变质岩及相关石英脉的地质研究和结构分析:对埃及努比亚地盾泛非火山活动的影响
乌姆阿纳布地区新元古代基底杂岩位于埃及东北沙漠(NED)赫尔格达市西南40公里处。基底岩石包括变质火山岩和巨大的花岗岩类岩体。变质火山发生区域变质作用,形成绿片岩-角闪岩相岩与带状铁地层互层。乌姆阿纳布变质火山构造分析表明,该地区存在多期构造变形,每期构造变形都有自己的作用和样式。发育发育约东西向、向南倾斜60º~ 80º的片岩,轴向面偏斜亚垂向nnw方向发育不对称褶皱。利用GArcmB软件对变质火山脉体进行了构造分析,确定了古应力反演,显示出在两种应力下形成的两组脉体。两簇的应力比(Φ)= (σ 2 - σ 3) / (σ 1 - σ 3)分别为~0.39和~0.16,表明两种应力状态。脉壁应力比值表明,在脉壁形成时,寄主岩石处于低至中等构造应力作用下。此外,利用Rf/φ方法估算了变质火山的有限应变结果(变化趋势为N73º~ 88ºE),证实了变质火山受低至中度变形影响的观点。伸展矿物线理和BIF具有ENE-WSW - E-W的趋势,支持最古老的缩短事件(D1),这被认为是与泛非逆冲作用相关的NNW-SSE早期变形阶段。
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