The Lamuchang Thallium deposit occurs in the core and near the core of the ne Lanmuchang anticline, and is controlled by NE-SW faults, which have relationship with the Lanmuchang anticline.
滥木厂铊矿床产于ne向滥木厂鼻状背斜核部和近核部，并严格受控于与背斜关系密切的NE向断裂组。
Controlled by structure trap, ore body located in the core of the brachyanticline or pitch part of plunging anticline which was intersected by high angle longitudinal fault.
矿体具体受断裂交汇部位附近的次级短轴背斜轴部、倾伏背斜的倾伏端及其翼部被纵向陡倾角断裂构造所切穿的部位控制，是断裂导矿与背斜构造圈闭的体现。
There are strong heterogeneous characteristics of reservoir property between the core and limbs of the Kela-2 anticline, although they are in the same structure.
尽管处于同一构造样式内，克拉2背斜构造核部和两翼部位的储集层物性仍表现出明显的差异。
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