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作 者:朱书阶
机构地区:[1]中煤科工集团西安研究院,陕西西安710054
出 处:《中国煤炭地质》2011年第5期49-52,共4页Coal Geology of China
基 金:国家重大基础研究发展计划(973计划)项目(2006CB202208);大型油气田及煤层气开发科技重大专项项目(2008ZX05040-003)
摘 要:三维地震勘探技术已经成为解决矿区煤与瓦斯突出区域的重要手段,而突出区域特殊的地球物理特征为这种技术的实施提供了可能。实验室测试资料表明:突出煤层的地震波速度约为正常煤层的1/3,因此煤层突出区域具备利用地震技术进行检测的物性条件;地震正演模拟结果显示,煤与瓦斯突出部位的煤层地震反射波的传播时间、能量和频率特征,与正常煤层存在明显差异;实际资料表明,煤层突出地段在地震资料上出现地震波至时间加长、振幅减弱、频率降低等特征,这与理论研究结果是一致的。初步分析认为:地震资料的时间、振幅和频率变化等特征,可以作为利用地面地震圈定煤与瓦斯突出区域的辅助标志。The 3D seismic prospecting has been proven an important means to identify mine area coal and gas outburst,while the special geophysical characteristics provide the possibility for the technology's feasibility in that kind of areas.Laboratory tested data have demonstrated that: wave velocity in outburst coal seams is about 1/3 of that in normal coal seams,thus coal seams with outburst hazard possess physical property conditions to use the technology.The seismic forward modeling has shown: reflection propagation time,energy and frequency characteristics in coal seams in coal and gas outburst position are distinctly different from those in normal coal seams.Actual data have shown that characteristics of postponing time of arrival,amplitude weakening and frequency lowering present on seismic data in outburst sector,that are accord with theoretical results.Preliminary analysis has considered that time,amplitude and frequency variation characteristics on seismic data can be auxiliary indications to delineate outburst areas.
分 类 号:P631.4[天文地球—地质矿产勘探]
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