全张量重力数据交叉梯度联合反演技术研究
详细信息 查看官网全文
- 论文作者：乔中坤 ; 黄大年 ; 赵思敏 ; 张元元
- 年：2016
- 作者机构：吉林大学;四川农业大学;
- 会议召开时间：2016-10-15
- 会议录名称：2016中国地球科学联合学术年会论文集（二十一）——专题43：工程地球物理技术进展与应用、专题44：地球重力场及其地学应用
- 语种：中文
- 分类号：P631.1
- 学会代码：ZGDW
- 会议名称：2016中国地球科学联合学术年会
- 会议地点：中国北京
- 主办单位：中国地球物理学会、中国地震学会、全国岩石学与地球动力学研讨会组委会、中国地质学会构造地质学与地球动力学专业委员会、中国地质学会区域地质与成矿专业委员会
- 学会名称：中国地球物理学会
- 页数：2
- 文件大小：1117k
- 原文格式：D
- 会议级别：全国
摘要
<正>重力勘探具有轻便,快捷,投入少的优点,广泛应用于研究地壳内部的结构、构造、探查固体矿产和油气资源分布,查明大型建筑工程基底的稳定性等。航空重力测量的出现大大提高了重力勘探效率,降低了勘探成本,能够快速完成条件恶劣地区大面积重力勘探。随着重力勘探测量仪器精度的提高以及GPS技术的进步,高精度的航空、海洋重力梯度测量技术得到迅速发展。目前,国外的重力梯度测量技术已经发展到商用阶段。全张量测量始于20世纪90年代,是一种非常有效的地球物理探测手段。全张量探测技术以其信
引文
[1]Bosch M,Mc Caughey J.Joint inversion of gravity and magnetic data under lithological constrants[J].The Leading Edge,2001,20(8):877-881.
[2]Luis A G,Max A M.Joint two-dimensional DC resistivity and seismic travel time inversion with cross-gradients constraints[J].JOURNAL OF GEOPHYSICAL research,2004,109(bo3311).
[3]Luis A G.Joint two-dimensional inversion of geoelectromagnetic and seismic refraction data with cross-gradients constraint[D].England:Lancaster University,2004.
[4]Heincke B,Hobbs R.Joint inversion of MT,gravity and seismic data applied to sub-basalt imaging.SEG Expanded Abstract,2006,25(1):784-787.
[5]Emilia Fregoso,Luis A.Gallardo.Cross-gradients joint 3d inversion with applications to gravity and magnetic data[J].GEOPHYSICS,2009,74(4):31-42.
[6]Luis A.Gallardo.Multiple cross-gradients joint inversion for geospectral imaging[J].GEOPHYSICAL RESEARCH LETTERS,2007,34,L 19301,doi:10.1029/2007 GL030409.
[7]Luis A.Gallardo,Max A.Meju.Joint two-dimensional cross-gradients imaging of magnetotelluric and seismic travel time data[J].Geophys,2007,169,1261-1272.
[8]Wenke,M.Geophysical Data Analysis:Discrete Inverse Theory[M].California:Academic Press,1984.
[9]Zelt,C.A.,P.J.Barton.Three-dimensional seismic refraction tomography:A comparison of two methods applied to data from the Faeroe Basin[J].Geophys,1998,Res.103,7187-7210.
[10]Spector A and Grant F S.Statistical models for interpreting aeromagnetic data[J].Geophysics,1970,35(2):293–302.
[11]Syberg F J R.A Fourier method for the regional residual problem of potential fields[J].Geophysical Prospecting,1972,20:47.
[12]Zurflueh E G.Application of two-dimensional linear wave-length filtering[J].Geophysics,1967,32:1015–1035.
[13]熊盛青.我国航空重磁勘探技术现状与发展趋势[J].地球物理学进展,2009,24(1):113-117.
[14]史建民,韩吉龙,胡鑫.黑龙江大兴安岭地区航磁异常的筛选与查证经验[J].世界地质,2013,32(4):832-839.
[15]贺日政,高锐,郑洪伟.隐伏在青藏高原中部的东西走向断裂的航磁异常场特征及其意义[J].吉林大学学报:地球科学版,2007,37(5):1002-1008.
[16]马国庆,杜晓娟,李丽丽,等.梯度反褶积法及其在矿产勘探中的应用[J].吉林大学学报(地球科学版),2013,43(1):259-266.
[17]P.Leliak,Identification and Evaluation of Magnetic Field Sources of Magnetic Airborne Detector MAD Equipped Aircraft,IRA Transactions on Airspace and Navigational Electronics,Volume 8,P.95-105,September 1961.
[18]B.W.Leach,Automatic Aeromagnetic Compensation,National Research Council of Canada,National Aeronautical laboratory LTR-FR69,March 1979a.
[19]B.W.Leach,Aeromagnetic compensation as a linear regression problem,Information linkage between applied mathematics and industry II:Academic Press Inc.,1979b.
[20]刘晓杰.航磁补偿技术研究[D].吉林:吉林大学,2009.
[21]王俊.基于交叉梯度重磁联合反演方法技术研究[D].中国地质大学(北京),2014.
[22]陈晓红.基于交叉梯度函数的重震同步联合反演方法研究[D].中国石油大学(华东),2013.
[2]Luis A G,Max A M.Joint two-dimensional DC resistivity and seismic travel time inversion with cross-gradients constraints[J].JOURNAL OF GEOPHYSICAL research,2004,109(bo3311).
[3]Luis A G.Joint two-dimensional inversion of geoelectromagnetic and seismic refraction data with cross-gradients constraint[D].England:Lancaster University,2004.
[4]Heincke B,Hobbs R.Joint inversion of MT,gravity and seismic data applied to sub-basalt imaging.SEG Expanded Abstract,2006,25(1):784-787.
[5]Emilia Fregoso,Luis A.Gallardo.Cross-gradients joint 3d inversion with applications to gravity and magnetic data[J].GEOPHYSICS,2009,74(4):31-42.
[6]Luis A.Gallardo.Multiple cross-gradients joint inversion for geospectral imaging[J].GEOPHYSICAL RESEARCH LETTERS,2007,34,L 19301,doi:10.1029/2007 GL030409.
[7]Luis A.Gallardo,Max A.Meju.Joint two-dimensional cross-gradients imaging of magnetotelluric and seismic travel time data[J].Geophys,2007,169,1261-1272.
[8]Wenke,M.Geophysical Data Analysis:Discrete Inverse Theory[M].California:Academic Press,1984.
[9]Zelt,C.A.,P.J.Barton.Three-dimensional seismic refraction tomography:A comparison of two methods applied to data from the Faeroe Basin[J].Geophys,1998,Res.103,7187-7210.
[10]Spector A and Grant F S.Statistical models for interpreting aeromagnetic data[J].Geophysics,1970,35(2):293–302.
[11]Syberg F J R.A Fourier method for the regional residual problem of potential fields[J].Geophysical Prospecting,1972,20:47.
[12]Zurflueh E G.Application of two-dimensional linear wave-length filtering[J].Geophysics,1967,32:1015–1035.
[13]熊盛青.我国航空重磁勘探技术现状与发展趋势[J].地球物理学进展,2009,24(1):113-117.
[14]史建民,韩吉龙,胡鑫.黑龙江大兴安岭地区航磁异常的筛选与查证经验[J].世界地质,2013,32(4):832-839.
[15]贺日政,高锐,郑洪伟.隐伏在青藏高原中部的东西走向断裂的航磁异常场特征及其意义[J].吉林大学学报:地球科学版,2007,37(5):1002-1008.
[16]马国庆,杜晓娟,李丽丽,等.梯度反褶积法及其在矿产勘探中的应用[J].吉林大学学报(地球科学版),2013,43(1):259-266.
[17]P.Leliak,Identification and Evaluation of Magnetic Field Sources of Magnetic Airborne Detector MAD Equipped Aircraft,IRA Transactions on Airspace and Navigational Electronics,Volume 8,P.95-105,September 1961.
[18]B.W.Leach,Automatic Aeromagnetic Compensation,National Research Council of Canada,National Aeronautical laboratory LTR-FR69,March 1979a.
[19]B.W.Leach,Aeromagnetic compensation as a linear regression problem,Information linkage between applied mathematics and industry II:Academic Press Inc.,1979b.
[20]刘晓杰.航磁补偿技术研究[D].吉林:吉林大学,2009.
[21]王俊.基于交叉梯度重磁联合反演方法技术研究[D].中国地质大学(北京),2014.
[22]陈晓红.基于交叉梯度函数的重震同步联合反演方法研究[D].中国石油大学(华东),2013.