长期以来，甭哥正长岩体被认为是印度—欧亚板块碰撞引起的走滑剪切构造所控制的碱性岩浆活动的产物。
Bengge syenites has been always regarded as the product of alkaline magma activity controlled by the strike-slip structures caused by collision between Yindia and Euroasia.
通过分析发现，影响该区崩滑形成的因素有区域地质构造、地层岩性、地形地貌及气象水文条件。
The influence factors of collapse-slide are regional tectonic, stratum lithologic, geomorphic, meteorological and hydrographic characteristics of Changbai Mountain.
通过调研发现，许多推、滑覆体之下掩覆了大片含煤岩系，为寻找隐伏煤田带来了新的希望，南、北构造“交汇带”也是钴多金属矿床较理想的找矿靶区。
So, the tectonic pattern of thrusting in the northern part and slipping in the southern part are founded. According to the geological survey, a large scale of coal-bearing serie…
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