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Origin Analysis on Breccia of the Lower Mantou Fromation of Cambrian System in Reservoir Area in Hekou Village

机译:河口村库区寒武系下System头组角砾岩成因分析。

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Mantou Fromation of Cambrian System is one of the major strata developed in the reservoir and dam area. It belongs to Mantou Fromation of Cambrian System, which is closely related to the engineering geology and leakage feature of the reservoir, and the breccia is found to distribute in many places in the lower part Mantou Fromation. Geological body and lithological features of breccias are described in significant detail in this paper. The breccia of the lower Mantou Fromation can be classified into 2 types. Origin of the two types of the breccia was analyzed on basis of the result of the sedimentary environment study and mineral chemical composition testing. One type of the breccia was formed in the lower incompetent rock layers of Mantou Fromation, formed by weathering and unloading at the offshore slopes; the other type was developed in the brittle rocks in the lower portion of Mantou Fromation as a result of tectonic movements. This origin analysis offers a basis for the assessment on engineering geological issues and reservoir leakage in the reservoir areas.
机译:寒武系的曼头河系是水库和水坝地区发展的主要地层之一。它属于寒武系的曼头地层,与储层的工程地质和渗漏特征密切相关,角砾岩分布在曼头地层的下部。角砾岩的地质体和岩性特征在本文中有详尽的描述。曼图河下部的角砾岩可分为两种类型。根据沉积环境研究和矿物化学成分测试的结果,分析了两种角砾岩的成因。一种类型的角砾岩形成于Mantou Fromation下部不称职的岩石层中,是通过在海上斜坡上风化和卸载形成的。另一种类型是由于构造运动在芒头河谷下部的脆性岩石中发育的。该成因分析为评估工程地质问题和库区的储层渗漏提供了基础。

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