D-InSAR技术及其在活断层运动学研究中的应用
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摘要
D-InSAR技术作为InSAR观测的重要方面,可以对地表形变进行比较精确的探测。随着目前国内外利用InSAR观测技术对地形测绘、活断裂(主要是活断层发育地区的地震同震形变)、地面沉降、滑坡、火山爆发、冰川运动等所进行的一系列探索和实践,该技术的研究也开始从萌芽向更加广泛和纵深发展。本文在介绍InSAR技术基本原理的同时,重点介绍目前该项技术在活断裂运动学研究中的应用以及未来的研究展望。
DInSAR is an important part of InSAR observation With DInSAR observation the precise crustal deformation can be obtained As employed in the reserch on terrain mapping, active faults kinematics (especially on coseismic deformation), land subsidence, landslide, volcano eruption, glacier motion, InSAR will be used in more extensive field As the basic theory is depicted, this paper mainly focuses in how to use InSAR in the research on the active faults and its prospect
DInSAR is an important part of InSAR observation With DInSAR observation the precise crustal deformation can be obtained As employed in the reserch on terrain mapping, active faults kinematics (especially on coseismic deformation), land subsidence, landslide, volcano eruption, glacier motion, InSAR will be used in more extensive field As the basic theory is depicted, this paper mainly focuses in how to use InSAR in the research on the active faults and its prospect
引文
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[4] 单新建,等.利用差分干涉雷达测量技术(D-InSAR)提取同震形变场[J].地震学报,2002,24(04):413-420.
[5] 王超,刘智,张红.张北—尚义地震同震形变场雷达差分干涉测量[J].科学通报,2000,45(23):2500-2553.
[6] 张红,王超,刘智.获取张北地震同震形变场的差分干涉测量技术[J].中国图像图形学报,2002,5(A6):497-500.
[7] E.J.Fielding,R.G.Blom,andR.M.Goldstein.RapidsubsidenceoveroilfieldsmeasuredbySARinterferometry[J].Geophys.Res.Lett,1998,25(7):3215-3218.
[8] D.Massonnet,T.Holzer,andH.Vadon.LandsubsidencecausebyEastMesageothermalfield,California,ob-servedusingSARinterferometry[J].Geophys.Res.Lett,1997,24(8):901-904.
[9] D.Massonnet,P.Briol,andA.Arnaud.DeflationofMountEtnamonitoredbyspaceborneradarinterfermetrry[J].Nature,1995,375:567-570.
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[11] H.Vadon,andF.Sigmundsson.Crustaldeformationfrom1992to1995atthemidatlanticridge.SouthwestIceland,mappedbysatelliteradarinterferometry[J].Science,1997,275(5297):193-197.
[12] B.Fruneau,J.Achache,andC.Delacourt.ObservationandmodelingoftheSaint-EtiennedeTineelandslideusingSARinterferometry[J].Tectonophys,1996,265(3-4):181-190.
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[14] 王超,杨清友.干涉雷达在地学研究中的应用[J].遥感技术与应用,1997,12(4):16-42.
[15] 袁孝康.干涉式合成孔径雷达测量技术[J].上海航天,1998,(5):20-26.
[16] 刘国祥,等.极具潜力的空间对地观测新技术——合成孔径雷达干涉[J].地球科学进展,2000,15(6):734-740.
[17] 徐锡伟,等.中国大陆地表破裂型潜在震源区的地震地质综合判定[J].震情研究,2000,44(1):14-26.
[18] 徐锡伟,等.张北-尚义地震的地震构造环境与宏观破坏特征[J].地震地质,1998,20(2):135-145.
[19] 王超,张红,于勇,等.雷达差分干涉测量[J].地理学与国土研究,2002,18(3):13-17.
[20] R.Bürgmann,E.Fielding,J.Sukhatme.SlipalongtheHaywardfault,California,estimatedfromspace-basedsyn-theticradarinterferometry[J].Geology,1998,26(6):559-562.
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