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The Characteristics and the Dominant Factor of Fracture Development of the Lower Silurian Longmaxi Formation Black Shale in Sangzhi

机译:Sangzhi下氏硅兰龙马西形成黑色页岩骨折开发的特征及显性因素

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Based on the analysis of tectonic faults in Sangzhi area, black shales fracture characteristics and controlling factors of the Longmaxi formation of Lower Silurian are studied. That fracture distribution of the study area is mainly controlled by fault, where the NE-trending fault system plays the most significant role. Fracture zones are located in the anticlinal axis, as well as at the stress concentration, such as near the fault or in intersection of different fault zone. Dispersion of fracture strike and its density are controlled by the fault line, fracture develops near the fault line, which strike is mainly north-east. It contains high content of brittle mineral which becomes friable rock and has well-developed fracture.
机译:基于Sangzhi地区的构造故障分析,研究了较低硅藻土龙马西骨折特性及控制因素。该研究区域的断裂分布主要受到故障的控制,其中NE趋势故障系统发挥着最大的作用。骨折区域位于横向轴线,以及应力集中,如附近的断层或不同断层区域的交叉点。断裂撞击的分散和其密度受到断层线的控制,断裂线在故障线附近产生,罢工主要是东北部。它含有高含量的脆性矿物质,成为易碎的岩石并具有发达的骨折。

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