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Geological Mapping, Structural Setting and Petrographic Description of the Archean Volcanic Rocks of Mnanka Area, North Mara

机译:地质映射,北玛拉庞纳地区的阿臣火山岩岩石的结构和岩体描述

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The Mnanka area is situated within the Musoma Mara Greenstone Belt, the area is near to Nyabigena, Gokona and Nyabirama gold mines. Mnanka area comprises of the sequence of predominant rhyolitic volcanic rocks, chert and metasediments. Gold mineralizations in Mnanka area is structure controlled and occur mainly as hydrothermal disseminated intrusion related deposits. Hence the predominant observed structures are joints and flow banding. Measurements from flow banding plotted on stereonets using win-TENSOR software has provided an estimate for the general strike of the area lying 070° to 100° dipping at an average range angle of 70° to 85° while data from joints plotted on stereonets suggest multiple deformation events one of which conforms to the East Africa Rift System (striking WSW-ENE, NNE-SSW and N-S).
机译:Mnanka地区位于Maroma Mara Greenstone Belt,该地区临近Nyabigena,Gokona和Nyabirama金矿。 Mnanka地区包括主要的卟啉火山岩,Chert和MetaseDiment的序列。 Mnanka地区的金矿化是结构控制的,主要作为水热传播侵入相关沉积物。 因此,主要观察到的结构是关节和流动绑带。 使用Win-Tensod软件绘制的流动带的测量提供了使用Win-TensoL软件的一般击球的估计,该区域将070°与70°至85°的平均范围角度浸渍,而来自绘制的关节数据的数据表明多个 变形事件之一符合东非裂谷系统(醒目WSW-ENE,NNE-SSW和NS)。

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