新疆布腊图勘查区地震磁法勘探煤层火烧边界
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
煤层在燃烧过程中,其围岩受到高温烘烤,致使煤层上、下部围岩裂隙发育,失去了形成层状地震反射的条件,同时在磁性、导电性等方面物理性质也发生显著变化,为地震勘探及磁法勘探的实施提供了理论依据。该文通过实例介绍了利用三维地震勘探和磁法勘探相结合准确圈定各主采煤层火烧区边界的方法及经验。
During the combustion process of coal strata,under the effect of high temperature,surrounding rocks in the upper and lower part of coal strata developed and lost the conditions for layered seismic reflection.At the same time,there are noticeable changes regarding physical properties,such as magnetism and electric conductivity.It will provide theory basis for seismic surveying and magnetic surveying.In this paper,through practical examples,methods and experiences for precisely delineating boundaries of burning areas in each main coal strata combining seismic surveying and magnetic surveying together have been introduced.
引文
[1]张威.山东煤田地震勘探及展望[J].山东地质,1990,6(2):79-86.
    [2]黄群.综合物探方法在煤矿火烧区探测中的应用[J].山西科技,2011,(2):81-83.
    [3]曾融生,陆涵行,丁志峰.从地震折射和反射剖面结果讨论唐山地震成因[J].地球物理学报,1988,(4):23-38.
    [4]陆基孟.地震勘探原理[M].北京:石油大学出版社,2005.
    [5]MT/T897-2000.煤炭煤层气地震勘探规范[S].2000.
    ①山东省煤田地质局物探测量队,刘正风,新疆和什托洛盖煤田和布克赛尔蒙古自治县布腊图勘查区三维地震勘探报告,2010年。

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心