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基于微震分析法的特厚煤层导水裂缝带高度研究
Research on Height of Water-induced Fissure Zone in Mining Extremely-thick Coal-seam by Micro-seismic Method
【摘要】 针对老虎台矿区特厚煤层、断层构造较多、开采条件复杂等特点,通过应用微震分析法对83002工作面的导水裂缝带高度进行了研究。根据对微震事件分布规律,确定了83002工作面导水裂缝带高度,并应用现场可控源音频大地电磁法(CSAMT法)对其进行了验证,结果基本一致,可以确定所得上覆岩体导水裂缝带范围和高度的合理性,为后续开采的设计和安全防护提供了指导。
【Abstract】 Aiming at extremely thick coal-seam,abundant faults and complex mining conditions of Laohutai Colliery,micro-seismic monitoring system was applied to obtaining the height of water-induced fissure zone of 83002 mining face according to micro-seismic matters distribution rule.CSAMT was used to prove the height and range of water-induced fissure zone was rational.Micro-seismic method could provide reference for mining design and safety.
【关键词】 微震分析法;
特厚煤层;
导水裂缝带;
CSAMT;
【Key words】 micro-seismic analysis; extremely thick coal-seam; water-induced fissure zone; CSAMT;
【Key words】 micro-seismic analysis; extremely thick coal-seam; water-induced fissure zone; CSAMT;
【基金】 国家科技重大专项(2011ZX05040-002);国家国际科技合作专项(0S2012ZR0400)
- 【文献出处】 煤矿开采 ,Coal Mining Technology , 编辑部邮箱 ,2012年06期
- 【分类号】TD325.4
- 【被引频次】3
- 【下载频次】103