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Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution

机译:东非造山带的造山带样式:新元古代至寒武纪构造演化的回顾

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摘要

Condensed timetable of major geologic events in the East African Orogen. Opening of the Mozambique Ocean and formation of rift basins in Zambia, Malawi, Mozambique and SW Madagascar was accompanied by emplacement of anorthosite melt in extending crust. A first phase of ocean closure and accretion of terranes defines the East African Orogeny. The second orogen phase, Kuungan Orogeny, mainly affected the southern parts of east Africa and Madagascar. Both shortening events were followed by extension phases that were accompanied by emplacement of late- to post-tectonic granitoids. EGCD: Eastern Granulite–Cabo Delgado Nappe Complex; Madag: Madagascar; Ub–Us: Usagaran/Ubendian Belts; WG: Western Granulite Be IB (Z–M): Irumide Belt of Zambia and Malawi; IB (M): Irumide Belt of Mozambique.
机译:东非造山带主要地质事件的简明时间表。莫桑比克海洋的开放以及赞比亚,马拉维,莫桑比克和马达加斯加西南部的裂谷盆地的形成,伴随着钙铁矿熔体在扩展地壳中的进入。海洋封闭和增生的第一阶段定义了东非造山带。第二造山带相,“昆刚造山带”,主要影响到东非南部和马达加斯加。两次缩短事件之后都是延伸期,并伴有晚期至构造后的花岗岩类。 EGCD:东部花岗岩-卡波德尔加多纳皮复合体;马达格:马达加斯加; Ub–Us:Usagaran / Ubendian Belts; WG:西部花岗石带; IB(Z–M):赞比亚和马拉维的伊鲁米德带; IB(M):莫桑比克的伊鲁米德腰带。<!-fig ft0-> <!-fig @ position =“ anchor” mode = article f4-> <!-fig mode =“ anchred” f5-- > <!-fig / graphic | fig / alternatives / graphic mode =“ anchored” m1->

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