基于CORONA像对的活动构造变形参数定量提取
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摘要
为了高效提取活动构造研究的定量参数,利用美国解密的2m分辨率CORONAKH-4B卫星立体像对,实现了在JX4C数字摄影测量系统的立体测图,并通过影像匹配的方法建立数字高程模型(DEM)和数字正射影像(DOM).通过以上方法,以南天山库车冲断褶皱带为例,利用覆盖该区的影像,识别由活动断层和活动褶皱造成的第四纪沉积物的变形,提取地表变形参数,结合地震资料和野外测量,分析地表变形特征的深部构造机理.结果表明,经过处理的CORONAKH-4B像对可以在数字摄影测量系统下矢量测图,相对定向精度在0.01mm左右,绝对定向精度在10m左右.测量精度能够满足活动构造定量分析所需.该方法在地势复杂、人迹罕至区域研究中更具优势.
In order to efficiently extract quantitative parameters in active tectonics research,JX4C digital photogrammetric system has been used to found stereo model based on CORONA KH-4B stereo pairs with 2 m resolution,which were declassified in 1995 by USA for scientific purpose.Meanwhile,large scale digital elevation model (DEM) and digital orthophoto mapping (DOM) have been formed.These processing techniques are applied in a case study of the Kuqa fold-and-thrust belt in southern Tianshan,China,to quantitatively analyze the Kumugeliemu active fault and the Qiulitage active fault-related folds,considering the seismic reflection profiles therein and data from field measurements.Results show that the CORONA stereo pairs can be used in JX4C digital photogrammetric system,and root mean square error (RMS) of relative orientation is about 0.01 mm,while absolute orientation is about 10 m.Some parameters for deformation of river terrace and fault and fold scarps are identified and measured,which are helpful to reveal the characters of active tectonics.The processing techniques are feasible and effective particularly in remote settings with complex topology and the measurement precision can meet the requirement for analysis of active tectonics.
In order to efficiently extract quantitative parameters in active tectonics research,JX4C digital photogrammetric system has been used to found stereo model based on CORONA KH-4B stereo pairs with 2 m resolution,which were declassified in 1995 by USA for scientific purpose.Meanwhile,large scale digital elevation model (DEM) and digital orthophoto mapping (DOM) have been formed.These processing techniques are applied in a case study of the Kuqa fold-and-thrust belt in southern Tianshan,China,to quantitatively analyze the Kumugeliemu active fault and the Qiulitage active fault-related folds,considering the seismic reflection profiles therein and data from field measurements.Results show that the CORONA stereo pairs can be used in JX4C digital photogrammetric system,and root mean square error (RMS) of relative orientation is about 0.01 mm,while absolute orientation is about 10 m.Some parameters for deformation of river terrace and fault and fold scarps are identified and measured,which are helpful to reveal the characters of active tectonics.The processing techniques are feasible and effective particularly in remote settings with complex topology and the measurement precision can meet the requirement for analysis of active tectonics.
引文
Alt maier,A.,Kany,C.,2002.Digital surface model genera-tion from CORONA satellite i mages.ISPRS Journalof Photogrammetry&Remote Sensing,56(4):221-235.doi:10.1016/S0924-2716(02)00046-1
Bai,M.X.,1998.Data of valley terraces in Xinjiang.InlandEarthquake,12(1):13-19(in Chinese with Englishabstract).
Chen,J.,Scharer,K.M.,Burbank,D.W.,et al.,2005.Kine-matic models of fluvial terraces over active fault-relatedfolds:constraints on the growth mechanism and kine-matics.Seismology and Geology,17(4):513-529(inChinese with English abstract).
Chen,L.C.,Chen,G.H.,Chen,L.Z.,et al.,2006.ETMi m-age characteristics and interpretation of active tectonicsof the area around the Kalpingtag thrust system.Seis-mology and Geology,28(2):289-298(in Chinese withEnglish abstract).
Chen,N.H.,Wang,X.,Yang,S.F.,2007.Quantitative ex-traction of shallow stratuminformation based on CO-RONAi magery.Journal of Zhejiang University(En-gineering Science),41(4):662-667(in Chinese withEnglish abstract).
Deng,Q.D.,Chen,L.C.,Ran,Y.K.,2004.Quantitativestudies and applications of active tectonics.Earth Sci-ence Frontiers,11(4):383-392(in Chinese with Eng-lish abstract).
Deng,Q.D.,Feng,X.Y.,Zhang,P.Z.,et al.,2000.Activetectonics in Tianshan.Seismological Press,Beijing(inChinese).
Deng,Q.D.,Zhang,P.Z.,Ran,Y.K.,et al.,2003.Basiccharacteristics of active tectonics of China.Science inChina(Series D),46(4):356-372.
Fan,X.T.,Lu,H.F.,Guo,H.D.,et al.,2000.Neotectonicanalysis of the Kuqa foreland thrust belt by using re-mote sensing data.Geological Review,46(5):499-506(in Chinese with English abstract).
Hooper,D.M.,Bursik,M.I.,Webb,F.H.,2003.Applica-tion of high-resolution,interferometric DEMs to geo-morphic studies of fault scarps,Fish Lake Valley,Ne-vada-California,USA.Remote Sensing of Environment,84:255-267.doi:10.1016/S0034-4257(02)00110-4
Hubert-Ferrafi,A.,Suppe,J.,Gonzalez-Mieres,R.,et al.,2007.Mechanisms of active folding of the landscape(southern Tian Shan,China).Journal of GeophysicalResearch,112(B3),B03S09-1-B03S09-39.doi:10.1029/2006JB004362
Jordan,G.,Meijninger,B.M.L.,Hinsbergen,D.J.J.,etal.,2005.Extraction of morphotectonic features fromDEMs:development and applications for study areas inHungary and NW Greece.International Journal ofApplied Earth Observation and Geoinformation,7(3):163-182.doi:10.1016/j.jag.2005.03.003
Lu,H.F.,Jia,D.,Chen,C.M.,et al.,1999.Nature and ti mingof the Kuqa Cenozoic structures.Earth Science Frontiers,6(4):215-221(in Chinese with English abstract).
Lu,H.F.,Wang,S.L.,Suppe,J.,et al.,2002.Quaternaryfolding in the south piedmont of central segment ofTianshan mountains.Chinese Science Bulletin,47(21):1675-1679(in Chinese).
Schwartz,D.P.,1988.Geologic characterization of seismicsources:moving into the1990s.Geotechnical SpecialPublication,20:1-42.
Sohn,H.G.,Ki m,G.H.,Yom,J.H.,2004.Mathematical mod-elling of historical reconnaissance CORONA KH-4B I M-AGERY.The Photogrammetric Record,19(105):51-66.doi:10.1046/j.0031-868X.2003.00257.x
Suppe,J.,1983.Geometry and kinematics of fault-bend fold-ing.American Journal of Science,283(7):684-721.
Suppe,J.,Sabat,F.,Munoz,J.A.,et al.,1997.Bed-by-bedfold growth by kind-bend migration:sant Lorence deMorunys,eastern Paeness.Journal of Structural Geol-ogy,19(3-4):443-461.doi:10.1016/S0191-8141(96)00103-4
Tao,C.V.,Hu,Y.,2001.Acomprehensive study of the ra-tional function model for photogrammetric processing.Photogrammetric Engineering&Remote Sensing,67(12):1347-1357.
Walker,R.T.,2006.Aremote sensing study of active foldingand faulting in southern Kerman Province,S.E.Iran.Journal of Structural Geology,28(4):654-668.doi:10.1016/j.jsg.2005.12.014
Wallace,R.E.,1987.Grouping and migration of surface faul-ting and variations in slip rates onfaults inthe great ba-sin province.Bull.Seism.Soc.Am.,77(3):868-876.
Wang,X.,Ferrafi,A.H.,Suppe,J.,2001.Shortening ratesince Late Pleistocene in Aksu area,southern flank ofTianshan,China.Chinese Journal of Geology,36(2):195-202(in Chinese with English abstract).
Wang,X.,Jia,C.Z.,Yang,S.F.,et al.,2002.The ti me ofdeformation on the Kuqa fold-and-thrust belt in thesouthern Tianshan—based onthe Kuqa River area.ActaGeologica Sinica,76(1):55-63(in Chinese with Eng-lish abstract).
Wu,C.Y.,Shen,J.,Chen,J.B.,et al.,2006.Preli minarystudy of late Quaternary crustal shortening rate alongKuqa depressionin South Tianshan,Xinjiang.Seismolo-gy and Geology,28(2):279-288(in Chinese withEnglish abstract).
Zheng,W.J.,Guo,H.,Yuan,D.Y.,et al.,2002.Applicationof remote sensing i mage information in the research ofactive faults.Earthquake Research in Plateau,14(2):15-21(in Chinese with English abstract).
柏美祥,1998.新疆河谷阶地的年代.内陆地震,12(1):13-19.
陈杰,Scharer,K.M.,Burbank,D.W.,等,2005.利用河流阶地限定活动褶皱的类型和生长机制:运动学模型.地震地质,17(4):513-529.
陈立春,陈桂华,陈立泽,等,2006.柯坪塔格推覆系活动构造的ETM影像特征与解译.地震地质,28(2):289-298.
陈宁华,汪新,杨树锋,2007.基于CORONA影像的浅层地层信息定量提取.浙江大学学报(工学版),41(4):662-667.
邓起东,陈立春,冉勇康,2004.活动构造定量研究与应用.地学前缘,11(4):383-392.
邓起东,冯先岳,张培震,等,2000.天山活动构造,北京:地震出版社.
邓起东,张培震,冉勇康,等,2002.中国活动构造基本特征.中国科学(D辑),32(12):1020-1030.
范湘涛,卢华复,郭华东,等,2000.库车冲断带新构造遥感分析.地质论评,46(5):499-506.
卢华复,贾东,陈楚铭,等,1999.库车新生代构造性质和变形时间.地学前缘,6(4):215-221.
卢华复,王胜利,Suppe,J.,等,2002.天山中段南麓的第四纪褶皱作用.科学通报,47(21):1675-1679.
汪新,Ferrafi,A.H.,Suppe,J.,2001.晚更新世以来南天山阿克苏地区地壳缩短率.地质科学,36(2):195-202.
汪新,贾承造,杨树锋,等,2002.南天山库车冲断褶皱带构造变形时间——以库车河地区为例.地质学报,76(1):55-63.
吴传勇,沈军,陈建波,等,2006.新疆南天山库车坳陷晚第四纪以来地壳缩短速率的初步研究.地震地质,28(2):279-288.
郑文俊,郭华,袁道阳,等,2002.遥感影像信息在活动断裂研究中的应用.高原地震,14(2):15-21.
Bai,M.X.,1998.Data of valley terraces in Xinjiang.InlandEarthquake,12(1):13-19(in Chinese with Englishabstract).
Chen,J.,Scharer,K.M.,Burbank,D.W.,et al.,2005.Kine-matic models of fluvial terraces over active fault-relatedfolds:constraints on the growth mechanism and kine-matics.Seismology and Geology,17(4):513-529(inChinese with English abstract).
Chen,L.C.,Chen,G.H.,Chen,L.Z.,et al.,2006.ETMi m-age characteristics and interpretation of active tectonicsof the area around the Kalpingtag thrust system.Seis-mology and Geology,28(2):289-298(in Chinese withEnglish abstract).
Chen,N.H.,Wang,X.,Yang,S.F.,2007.Quantitative ex-traction of shallow stratuminformation based on CO-RONAi magery.Journal of Zhejiang University(En-gineering Science),41(4):662-667(in Chinese withEnglish abstract).
Deng,Q.D.,Chen,L.C.,Ran,Y.K.,2004.Quantitativestudies and applications of active tectonics.Earth Sci-ence Frontiers,11(4):383-392(in Chinese with Eng-lish abstract).
Deng,Q.D.,Feng,X.Y.,Zhang,P.Z.,et al.,2000.Activetectonics in Tianshan.Seismological Press,Beijing(inChinese).
Deng,Q.D.,Zhang,P.Z.,Ran,Y.K.,et al.,2003.Basiccharacteristics of active tectonics of China.Science inChina(Series D),46(4):356-372.
Fan,X.T.,Lu,H.F.,Guo,H.D.,et al.,2000.Neotectonicanalysis of the Kuqa foreland thrust belt by using re-mote sensing data.Geological Review,46(5):499-506(in Chinese with English abstract).
Hooper,D.M.,Bursik,M.I.,Webb,F.H.,2003.Applica-tion of high-resolution,interferometric DEMs to geo-morphic studies of fault scarps,Fish Lake Valley,Ne-vada-California,USA.Remote Sensing of Environment,84:255-267.doi:10.1016/S0034-4257(02)00110-4
Hubert-Ferrafi,A.,Suppe,J.,Gonzalez-Mieres,R.,et al.,2007.Mechanisms of active folding of the landscape(southern Tian Shan,China).Journal of GeophysicalResearch,112(B3),B03S09-1-B03S09-39.doi:10.1029/2006JB004362
Jordan,G.,Meijninger,B.M.L.,Hinsbergen,D.J.J.,etal.,2005.Extraction of morphotectonic features fromDEMs:development and applications for study areas inHungary and NW Greece.International Journal ofApplied Earth Observation and Geoinformation,7(3):163-182.doi:10.1016/j.jag.2005.03.003
Lu,H.F.,Jia,D.,Chen,C.M.,et al.,1999.Nature and ti mingof the Kuqa Cenozoic structures.Earth Science Frontiers,6(4):215-221(in Chinese with English abstract).
Lu,H.F.,Wang,S.L.,Suppe,J.,et al.,2002.Quaternaryfolding in the south piedmont of central segment ofTianshan mountains.Chinese Science Bulletin,47(21):1675-1679(in Chinese).
Schwartz,D.P.,1988.Geologic characterization of seismicsources:moving into the1990s.Geotechnical SpecialPublication,20:1-42.
Sohn,H.G.,Ki m,G.H.,Yom,J.H.,2004.Mathematical mod-elling of historical reconnaissance CORONA KH-4B I M-AGERY.The Photogrammetric Record,19(105):51-66.doi:10.1046/j.0031-868X.2003.00257.x
Suppe,J.,1983.Geometry and kinematics of fault-bend fold-ing.American Journal of Science,283(7):684-721.
Suppe,J.,Sabat,F.,Munoz,J.A.,et al.,1997.Bed-by-bedfold growth by kind-bend migration:sant Lorence deMorunys,eastern Paeness.Journal of Structural Geol-ogy,19(3-4):443-461.doi:10.1016/S0191-8141(96)00103-4
Tao,C.V.,Hu,Y.,2001.Acomprehensive study of the ra-tional function model for photogrammetric processing.Photogrammetric Engineering&Remote Sensing,67(12):1347-1357.
Walker,R.T.,2006.Aremote sensing study of active foldingand faulting in southern Kerman Province,S.E.Iran.Journal of Structural Geology,28(4):654-668.doi:10.1016/j.jsg.2005.12.014
Wallace,R.E.,1987.Grouping and migration of surface faul-ting and variations in slip rates onfaults inthe great ba-sin province.Bull.Seism.Soc.Am.,77(3):868-876.
Wang,X.,Ferrafi,A.H.,Suppe,J.,2001.Shortening ratesince Late Pleistocene in Aksu area,southern flank ofTianshan,China.Chinese Journal of Geology,36(2):195-202(in Chinese with English abstract).
Wang,X.,Jia,C.Z.,Yang,S.F.,et al.,2002.The ti me ofdeformation on the Kuqa fold-and-thrust belt in thesouthern Tianshan—based onthe Kuqa River area.ActaGeologica Sinica,76(1):55-63(in Chinese with Eng-lish abstract).
Wu,C.Y.,Shen,J.,Chen,J.B.,et al.,2006.Preli minarystudy of late Quaternary crustal shortening rate alongKuqa depressionin South Tianshan,Xinjiang.Seismolo-gy and Geology,28(2):279-288(in Chinese withEnglish abstract).
Zheng,W.J.,Guo,H.,Yuan,D.Y.,et al.,2002.Applicationof remote sensing i mage information in the research ofactive faults.Earthquake Research in Plateau,14(2):15-21(in Chinese with English abstract).
柏美祥,1998.新疆河谷阶地的年代.内陆地震,12(1):13-19.
陈杰,Scharer,K.M.,Burbank,D.W.,等,2005.利用河流阶地限定活动褶皱的类型和生长机制:运动学模型.地震地质,17(4):513-529.
陈立春,陈桂华,陈立泽,等,2006.柯坪塔格推覆系活动构造的ETM影像特征与解译.地震地质,28(2):289-298.
陈宁华,汪新,杨树锋,2007.基于CORONA影像的浅层地层信息定量提取.浙江大学学报(工学版),41(4):662-667.
邓起东,陈立春,冉勇康,2004.活动构造定量研究与应用.地学前缘,11(4):383-392.
邓起东,冯先岳,张培震,等,2000.天山活动构造,北京:地震出版社.
邓起东,张培震,冉勇康,等,2002.中国活动构造基本特征.中国科学(D辑),32(12):1020-1030.
范湘涛,卢华复,郭华东,等,2000.库车冲断带新构造遥感分析.地质论评,46(5):499-506.
卢华复,贾东,陈楚铭,等,1999.库车新生代构造性质和变形时间.地学前缘,6(4):215-221.
卢华复,王胜利,Suppe,J.,等,2002.天山中段南麓的第四纪褶皱作用.科学通报,47(21):1675-1679.
汪新,Ferrafi,A.H.,Suppe,J.,2001.晚更新世以来南天山阿克苏地区地壳缩短率.地质科学,36(2):195-202.
汪新,贾承造,杨树锋,等,2002.南天山库车冲断褶皱带构造变形时间——以库车河地区为例.地质学报,76(1):55-63.
吴传勇,沈军,陈建波,等,2006.新疆南天山库车坳陷晚第四纪以来地壳缩短速率的初步研究.地震地质,28(2):279-288.
郑文俊,郭华,袁道阳,等,2002.遥感影像信息在活动断裂研究中的应用.高原地震,14(2):15-21.
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