李增学, 李守春. 下花园煤矿层间滑动构造研究[J]. 煤田地质与勘探, 1990, 18(1): 21-24.
引用本文: 李增学, 李守春. 下花园煤矿层间滑动构造研究[J]. 煤田地质与勘探, 1990, 18(1): 21-24.
On the Intraformational Sliding Structure of Xiahuayuan Coal Mine[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 21-24.
Citation: On the Intraformational Sliding Structure of Xiahuayuan Coal Mine[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 21-24.

下花园煤矿层间滑动构造研究

On the Intraformational Sliding Structure of Xiahuayuan Coal Mine

  • 摘要: 在下花园煤矿十分发育的小构造是层间滑动构造,它是大型逆掩断层形成过程中派生的,研究和弄清其间的关系。对井田构造预测和指导煤层开采具有实际意义。

     

    Abstract: Small geological structures are well developed and complex in Xiahuayuan Coal mine, but medium-sized geological structures are less.These small structures are chiefly reverse faulf. wich smallthrow and asymmetrical, overturned secondary,wich are intraformational sliding structures produced by intraformational teclonism wich is derivative from the process that form the large 一scale overthrust. Research indicate that the distortion of the axis of Yudaishan syncline and its sophistjcated limbs lead to the complexity of small geological structure.To make clear the causal relationship betwees the small structure and syncline has realistic significance in guarding structural forecast and coal mining.

     

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