闽西南高陂煤矿区构造特征及其演化

Structural Feature and Its Evolution of Gaobei Coal Mine in Southwest of Fujian

通过高陂煤矿区构造特征分析,探讨了该区构造演化过程,即高陂矿区的褶皱主要是高陂向斜;对矿区起控制作用的断层是滑覆断层。印支晚期主要形成三条滑覆断层;燕山早期形成高陂向斜;燕山中晚期形成南北边界逆断层,形成了高陂向斜南高北低格局。

The paper anglyses the mine structural evolution process by the feature of Gaobei mine area. Gaobei Syncline is major fold, a lot of secondary fault later period Indo - China play a comtrol role to mine area mainly formed three decollement fault.