运用地震属性技术解释煤矿陷落柱
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摘要
通过对山西某煤矿两个三维勘探区煤层反射波的属性特征进行的提取,对陷落柱反射波等地震属性特征进行了深入分析、研究,结合已知地质资料,利用基于地震层间属性定量描述与识别陷落柱的最新解释技术对勘探区进行了精细解释。
By the extraction of coal seam reflection wave attributes of two three-dimensional exploration ares in a coal mine in Shanxi made a deep analysis of the fall-wave of the collapst columm est.seismic reflection attributes combined with known geological data,and based on the earthquake attribute quantitative description and the latest interpretation of recoganizing collapse column made a fine explaination for the exploration area.
By the extraction of coal seam reflection wave attributes of two three-dimensional exploration ares in a coal mine in Shanxi made a deep analysis of the fall-wave of the collapst columm est.seismic reflection attributes combined with known geological data,and based on the earthquake attribute quantitative description and the latest interpretation of recoganizing collapse column made a fine explaination for the exploration area.
引文
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[2]断层和地层特征的三维地震不连续性:相干数据体[J].国外油气勘探,1996,8(3):340-346.
[3]K.J.Marfurt et al.1998.3-D seismic attributes using a semblance-based coherency algorithm.Geophysics,63(4):1150-1165.
[4]用基于相似的相干算法计算三维地震属性[J].石油物探译丛,1999,(3):22-37.
[5]一种基于相似性的相干算法的三维地震属性分析[J].国外油气勘探,2000,12(1):31-48.
[6]李玲,等.用地震相干数据体进行断层自动解释[J].石油地球物理勘探,1998,33(增刊1):105-111.
[7]佘德平,等.相干数据体及其在三维地震解释中的应用[J].石油物探,1998,37(4):75-79.
[8]杜文凤.相干体技术在煤田三维地震勘探中的应用[J].煤田地质与勘探,1998,26(6):56-59.
[9]K.J.Marfurt et al.1999.Coherency calculation in the presence ofstructural dip.Geophysics,64(1):104-111.
[10]A.Gersztenkorn and K.J.Marfurt.1999.Eigenstructure-based co-herence computations as an aid to 3-D structural and stratigraphicmapping.Geophysics,64(5):1468-1479.
[11]杨振武.三维地震相干应用研究[J].物探化探计算技术,1999,21(4):367-371.
[12]林建东,等.煤田三维地震资料解释中的方差体技术[J].中国煤田地质,2000,12(4):57-59.
[13]佘德平,等.应用三维相干技术进行精细地震解释[J].石油物探,2000,39(2):83-88.
[14]王永刚,等.利用相干数据体检测断层与特殊岩性体[J].石油大学学报,2000,24(1):69-72.
[2]断层和地层特征的三维地震不连续性:相干数据体[J].国外油气勘探,1996,8(3):340-346.
[3]K.J.Marfurt et al.1998.3-D seismic attributes using a semblance-based coherency algorithm.Geophysics,63(4):1150-1165.
[4]用基于相似的相干算法计算三维地震属性[J].石油物探译丛,1999,(3):22-37.
[5]一种基于相似性的相干算法的三维地震属性分析[J].国外油气勘探,2000,12(1):31-48.
[6]李玲,等.用地震相干数据体进行断层自动解释[J].石油地球物理勘探,1998,33(增刊1):105-111.
[7]佘德平,等.相干数据体及其在三维地震解释中的应用[J].石油物探,1998,37(4):75-79.
[8]杜文凤.相干体技术在煤田三维地震勘探中的应用[J].煤田地质与勘探,1998,26(6):56-59.
[9]K.J.Marfurt et al.1999.Coherency calculation in the presence ofstructural dip.Geophysics,64(1):104-111.
[10]A.Gersztenkorn and K.J.Marfurt.1999.Eigenstructure-based co-herence computations as an aid to 3-D structural and stratigraphicmapping.Geophysics,64(5):1468-1479.
[11]杨振武.三维地震相干应用研究[J].物探化探计算技术,1999,21(4):367-371.
[12]林建东,等.煤田三维地震资料解释中的方差体技术[J].中国煤田地质,2000,12(4):57-59.
[13]佘德平,等.应用三维相干技术进行精细地震解释[J].石油物探,2000,39(2):83-88.
[14]王永刚,等.利用相干数据体检测断层与特殊岩性体[J].石油大学学报,2000,24(1):69-72.
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