朱小静. 热水矿区煤层煤化程度反序原因浅析[J]. 煤田地质与勘探, 1989, 17(4): 32-37.
引用本文: 朱小静. 热水矿区煤层煤化程度反序原因浅析[J]. 煤田地质与勘探, 1989, 17(4): 32-37.

热水矿区煤层煤化程度反序原因浅析

  • 摘要: 热水矿区煤层煤化程度上高下低呈现反序现象,其原因各说不一.笔者在前人工作基础上,通过野外调查和室内多种手段的测试,认为主要是热液作用的结果.

     

    Abstract: According to the demonstration of various engincering geological factors and several examples,the authors evaluate the engineerieg geological stability of coal roof and it is highly important for coal field design, construction and production.

     

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