东北地区构造分区与深断裂研究——基于重力场小波多尺度分解
|
摘要
基于东北地区的布格重力异常资料,通过小波多尺度分解,将重力异常分解为四阶.提取主要反映深断裂的重力异常2、3阶小波细节,利用不同方向的水平梯度,计算并强化深断裂的线性特征,解译出12条深断裂,同时,结合功率谱法、东北地区地震分布、震源机制解和地质信息推断断裂的下切深度和性质,结果表明:12条深断裂分别对应拼贴地块的缝合带和对东北地区盆地群的分布与演化有着明显控制作用的岩石圈断裂两类;深断裂体系主要方向为北东、北北东向且大多为走滑断层;提取主要反映深层块体异常的3、4阶小波细节并结合深断裂体系将研究区划分为五个重力场一级分区,并首次将额尔古纳块体和兴安块体分开.五个大区分别为额尔古纳块体、兴安块体、松嫩块体、佳木斯块体和华北板块;其中兴安块体又分为二连盆地、大兴安岭两个二级分区;松嫩块体又分为小兴安岭、松辽盆地、张广才岭三个二级分区;佳木斯块体又分为那丹哈达地体、三江盆地、桦南—穆棱三个二级分区,华北板块又分为辽东半岛、华北板块、北部断裂带三个二级分区,结果表明了研究区的基本构造格局.
Wavelet multi-scale analysis is applied to the research on Bouguer gravity field and the explanation of tectonic structure and deep faults in northeast China.Based on Bouguer gravity anomaly,the gravity field is decomposed into four scale by multi-scale wavelet decomposition method.Extracting the second and third order details which reflect the anomalies correlated with deep faults and enhancing faults' linear features by calculating the horizontal gradient in different directions.The results indicate 12 deep faults.Meanwhile,the paper interprets the characteristics of deep faults with the power spectrum method and the information of seism distribution,focal mechanism and geology.The result shows that 12 deep faults are divided into two types.One is the suture zone between massifs.The other plays a significant role in distribution and evolution of basin groups.Deep faults system has a predominant direction in NE,NNE and most of faults are strike-slip faults.According to the characteristics of wavelet multi-scale decomposition and the deep faults system,the paper divides the Bouguer gravity in to first-order and secondary anomaly regions and describes the characteristics of their Bouguer gravity fields.Xing' an massif and Erguena massif was first separated.The first-order gravity anomaly regions contains Erguena massif,Xing'an massif,Songnen massif,Kiamusze massif,Huabei massif.The secondary anomaly regions contains Erlian basin,Greater Khingan region,Lesser Khingan region,Songliao basin,Zhangguangcai region,Nadanhada block,Sanjiang basin,Huanan-muling region,Liaotung peninsula region,Huabei massif,Fracture zone.The result depicts the framework of tectonic units in northeast China.
Wavelet multi-scale analysis is applied to the research on Bouguer gravity field and the explanation of tectonic structure and deep faults in northeast China.Based on Bouguer gravity anomaly,the gravity field is decomposed into four scale by multi-scale wavelet decomposition method.Extracting the second and third order details which reflect the anomalies correlated with deep faults and enhancing faults' linear features by calculating the horizontal gradient in different directions.The results indicate 12 deep faults.Meanwhile,the paper interprets the characteristics of deep faults with the power spectrum method and the information of seism distribution,focal mechanism and geology.The result shows that 12 deep faults are divided into two types.One is the suture zone between massifs.The other plays a significant role in distribution and evolution of basin groups.Deep faults system has a predominant direction in NE,NNE and most of faults are strike-slip faults.According to the characteristics of wavelet multi-scale decomposition and the deep faults system,the paper divides the Bouguer gravity in to first-order and secondary anomaly regions and describes the characteristics of their Bouguer gravity fields.Xing' an massif and Erguena massif was first separated.The first-order gravity anomaly regions contains Erguena massif,Xing'an massif,Songnen massif,Kiamusze massif,Huabei massif.The secondary anomaly regions contains Erlian basin,Greater Khingan region,Lesser Khingan region,Songliao basin,Zhangguangcai region,Nadanhada block,Sanjiang basin,Huanan-muling region,Liaotung peninsula region,Huabei massif,Fracture zone.The result depicts the framework of tectonic units in northeast China.
引文
[1]谢鸣谦.拼贴板块构造及其驱动机理—中国东北及邻区的大地构造演化.北京:科学出版社,2000:1-260.Xie M Q.Amalgamating Plate Tectonic and its DrovedMechanism-tectonic Evolution of Northeast China andAdjacent Area(in Chinese).Beijing:Science Press,2000:1-260.
[2]Jia D C,Hu R Z,Lu Y,et al.Collision belt between theKhanka block and the North China block in the YanbianRegion,Northeast China.Journal of Asian Earth Sciences,2004,23(2):211-219.
[3]Lin W,Faure M,Nomade S,et al.Permian-Triassic amalgamationof Asia:Insights from Northeast China sutures and their placein the final collision of North China and Siberia.ComptesRendus Geoscience,2008,340(2-3):190-201.
[4]任纪舜,姜春发,张正坤等.中国大地构造及其演化.北京:科学出版社,1980.Ren J S,Jiang C F,Zhang Z K,et al.The GeotectonicEvolution of China(in Chinese).Beijing:Science Press,1980.
[5]杨宝俊,刘财,梁铁成.满洲里-绥芬河地学断面域内莫霍的基本特征.长春科技大学学报,1998,28(1):111-113Yang B J,Liu C,Liang T C.The Basic Character of Moho inManzhouli-Suifenhe geoscience transecct.Journal of ChangchunUniversity of Science and Technology(in Chinese),1998,28(1):111-113.
[6]傅为洲,杨宝俊,刘财等.中国满洲里-绥芬河地学断面地震学研究.长春科技大学学报,1998,28(2):206-212Fu W Z,Yang B J,Liu C,et al.Study on the seismology inManzhouli-Suifenhe geoscience transect of China.Journal ofChangchun University of Science and Technology(in Chinese),1998,2:206-212.
[7]张凤旭,张兴洲,张凤琴等.中国东北地区重力场研究—利用改进的三方向小子域滤波划分主构造线及大地构造单元.地球物理学报,2010,53(6):1475-1485.Zhang F X,Zhang X Z,Zhang F Q,et al.Study of gravityfield in Northeastern China area:Classification of mainstructure lines and tectonic units using the improved three-directional small subdomain filtering.Chinese J.Geophys.(inChinese),2010,53(6):1475-1485.
[8]张凤旭,邰振华,张兴洲等.中国东北地区重力场研究----剩余重力场与重点油气勘探盆地的关系及油气勘探新领域.地球物理学进展,2011,26(2):424-432.Zhang F X,Tai Z H,Zhang X Z,et al.Study of gravity fieldin Northeastern China area:The relationship between residualgravity field and major exploratory basins,and new areas ofoil-gas exploration.Progress in Geophys.(in Chinese),2011,26(2):424-432.
[9]杜晓娟,孟令顺,张明仁.利用重力场研究东北地区断裂分布及构造分区.地球科学与环境学报,2009,31(2):200-206.Du X J,Meng L S,Zhang M R.Research on fault distributionand tectonic divisions in northeast China in terms of gravityfield.Journal of Earth Sciences and Environment(in Chinese),2009,31(2):200-206.
[10]胡旭芝,徐鸣洁,谢晓安等.中国东北地区航磁特征及居里面分析.地球物理学报,2006,49(6):1674-1681.Hu X Z,Xu M J,Xie X A,et al.A characteristic analysis ofaeromagnetic anomalies and Curie point isotherms in NortheastChina.Chinese J.Geophys.(in Chinese),2006,49(6):1674-1681.
[11]江为为,周立宏,肖敦清等.东北地区重磁场与地壳结构特征.地球物理学进展,2006,21(3):730-738.Jiang W W,Zhou L H,Xiao D Q,et al.The characteristicsof crust structure and the gravity and magnetic fields innortheast region of China.Progress in Geophysics(inChinese),2006,21(3):730-738.
[12]涂广红,江为为,朱东英等.中国东北地区剩余重磁异常特征与地质构造及成矿带的关系.地球物理学进展,2006,21(3):746-755Tu G H,Jiang W W,Zhu D Y,et al.The relationshipsbetween the characteristics of Northeast China residualgravity and magnetic anomalies and geological tectonic&metallogenic belt.Progress in Geophysics(in Chinese),2006,21(3):746-755.
[13]田有,刘财,冯晅.中国东北地区地壳、上地幔速度结构及其对矿产能源形成的控制作用.地球物理学报,2011,54(2):407-414Tian Y,Liu C,Feng X.P-wave velocity structure of crustand upper mantle in Northeast China and its control on theformation of mineral and energy.Chinese J.Geophys.(inChinese),2011,54(2):407-414
[14]刘财,张海江,杨宝俊等.小波变换在高分辨率地震勘探数据处理中的应用.长春地质学院学报,1996,26(1):78-82Liu C,Zhang H J,Yang B J,et al.Application of wavelettransform to digital processing in high resolution seismicprospecting.Journal of Changchun University of EarthSciences(in Chinese),1996,26(1):78-82
[15]Fedi M,Quarta T.Wavelet analysis for the regional-residualand local separation of potential field anomalies.Geophys.Prospecting,1998,46(5):507-525.
[16]Ucan O N,Seker S,Albora A M,et al.Separation of magneticfields in geophysical studies using a 2-D multi-resolutionWavelet analysis approach.Balkan Geophys.Soc.,2000,3(3):53-58.
[17]侯遵择,杨文采.中国重力异常的小波变换与多尺度分析.地球物理学报,1997,40(1):85-95。Hou Z Z,Yang W C.Wavelet transform and multi-scaleanalysis on gravity anomalies of China.Chinese J.Geophys.(in Chinese),1997,40(1):85-95.
[18]侯遵择,杨文采,刘家琦.中国大陆地壳密度差异多尺度反演.地球物理学报,1998,41(5):641-651.Hou Z Z,Yang W C,Liu J Q.Multiscale inversion of thedensity contrast within the crust of China.Chinese J.Geophys.(in Chinese),1998,41(5).641-651.
[19]高德章,侯遵择,唐建.东海及邻区重力异常多尺度分解.地球物理学报,2000,43(6):842-849。Gao D Z,Hou Z Z,Tang J.Multiscale analysis of gravityanomalies on east china sea and adjacent regions.Chinese J.Geophys.(in Chinese),2000,43(6):842-849.
[20]Albora A M,U?an O N.Gravity anomaly separation using2-D wavelet approach and average depth calculation.DogusUniv.J.(in Chinese),2001,3:1-12.
[21]邱宁,何展翔,昌彦君.分析研究基于小波分析与谱分析提高重力异常的分辨能力.地球物理学进展,2007,22(1):112-120.Qiu N,He Z X,Chang Y J.Ability of improving gravityanomaly resolution based on multiresolution wavelet analysisand power spectrum analysis.Prog.Geophys.(in Chinese),2007,22(1):112-20.
[22]Xu Y,Hao T Y,Li Z W,et al.Regional gravity anomalyseparation using wavelet transform and spectrum analysis.Journal of Geophysics and Engineering,2009,6(3):279-287.
[23]金旭,杨宝俊.中国满洲里-绥芬河地学断面地球物理场及深部构造特征研究.北京:地震出版社,1994.Jin X,Yang B J.Study on Geophysical and Deep TectonicCharacters in Manzhouli-Suifenhe Geoscience Transect ofChina(in Chinese).Beijing:Seismological PublishingHouse,1994.
[24]张萍,蒋秀琴.辽宁地区震源机制解及应力场特征的研究.东北地震研究,2000,16(1):1-7.Zhang P,Jiang X Q.Study of focal mechanism solutions andstress field characteristics in Liaoning region.SeismologicalResearch of Northeast China(in Chinese),2000,16(1):1-7.
[25]崔效锋,谢富仁,赵建涛.中国及邻区震源机制解的分区特征.地震地质,2005,27(2):298-307.Cui X F,Xie F R,Zhao J T.The regional characteristics offocal mechanism solutions in China and its adjacent areas.Seismology and Geology(in Chinese),2005,27(2):298-307.
[26]杨文采.地球物理反演的理论与方法.北京:地质出版社,1997.Yang W C.The Theory and Method of Geophysics Inversion(in Chinese).Beijing:Geology Publishing House,1997.
[27]Spector A,Grant F S.Statistical models for interpretingaeromagnetic data.Geophysics,1970,35(2):293-302.
[28]徐鸣洁,王良书,钟锴等.塔里木盆地重磁场特征与基底结构分析.高校地质学报,2005,11(4):585-592.Xu M J,Wang L S,Zhong K,et al.Features of gravitationaland magnetic fields in the Tarim basin and basement structureanalysis.Geological Journal of China Universities(inChinese),2005,11(4):585-592.
[29]杨宇山,李媛媛,刘天佑等.小波细节的微分特征及其在重力场断裂分析中的应用.地质与勘探,2003,39(1):41-44.Yang Y S,Li Y Y,Liu T Y,et al.The differentialcharacteristic of the wavelet details and its application in faultanalysis of gravity field.Geology and Prospecting(inChinese),2003,39(1):41-44.
[30]张先,赵丽,刘天佑等.北京地区航磁异常的多尺度分解及断裂研究.地震学报,2006,28(5):504-512.Zhang X,Zhao L,Liu T Y,et al.Multi-scale waveletseparation of aeromagnetic anomaly and study of faults inBeijing area.Acta Seismologica Sinica(in Chinese),2006,28(5):504-512.
[31]王桂梁,琚宜文,郑孟林等.中国北部能源盆地构造.徐州:中国矿业大学出版社,2007.Wang G L,Ju Y W,Zheng M L,et al.Tectonics of EnergyResource Basins in the Northern China(in Chinese).Xuzhou:China University of Mining and Technology Press,2007.
[32]叶慧文,张兴洲,周裕文.从蓝片岩及蛇绿岩特点看满洲里—绥芬河断面岩石圈结构与演化.//张兴洲.中国满洲里—绥芬河地学断面域内岩石圈结构及其演化的地质研究.北京:地震出版社,1994:73-83.Ye H W,Zhang X Z,Zhou Y W.Petrological structure andevolution of Manzhouli-Suifenhe section seeing fromcharacters of blueschist and ophiolite.//Zhang X Z ed.Study on Petrological Structure and Evolution Characters ofManzhouli-Suifenhe Section(in Chinese).Beijing:Seismological Publishing House,1994:73-83.
[33]李瑞山.新林蛇绿岩.黑龙江地质,1991,2(1):19-32.Li R S.Xinling Ophiolite.Heilongjiang Geology(inChinese),1991,2(1):19-32.
[34]张贻侠,孙运生,张兴洲等.中国满洲里—绥芬河地学断面1:1000000说明书.北京:地质出版社,1998:1-53.Zhang Y X,Sun Y S,Zhang X Z,et al.The 1:1000000Specification of the Manzhouli-Suifenhe Geo-transect(inChinese).Beijing:Geological Publishing House,1998:1-53.
[35]王跃,张兴洲,宋海峰等.牡丹江地区黑龙江杂岩的变质变形特征.吉林大学学报(地球科学版),2009,39(6):1066-1072.Wang Y,Zhang X Z,Song H F,et al.The metamorphic anddeformed characteristics of the Heilongjiang Melange inMudanjiang Area.Journal of Jilin University(Earth ScienceEdition)(in Chinese),2009,39(6):1066-1072.
[36]姚立珣,汪进,李亚荣.用震源机制解确定东北地区地壳应力场.东北地震研究,1992,8(2):27-32.Yao L X,Wang J,Li Y R.Crust stress in northeasternregion of China.Seismological Research of Northeast China(in Chinese),1992,8(2):27-32.
[37]葛荣峰,张庆龙,解国爱等.郯庐断裂带北段及邻区现代地震活动性与应力状态.地震地质,2009,31(1):141-154.Ge R F,Zhang Q L,Xie G A,et al.Seismic activity andstress state of the northern Tanlu Fault zone and its adjacentareas.Seismology and Geology(in Chinese),2009,31(1):141-154.
[38]张萍,孙文福,苗春兰等.东北地区中强地震震源机制解分析.地震地磁观测与研究,2009,30(1):12-19.Zhang P,Sun W F,Miao C L,et al.Analysis of focal-mechanism solution of moderately strong earthquakes inNortheast China.Seismological and Geomagnetic Observationand Research(in Chinese),2009,30(1):12-19.
[39]迟元林等著.松辽盆地深部结构及成盆动力学与油气聚集.北京:石油工业出版社,2002:1-274.Chi Y L,et al.Deep Structure,Basin Dynamics and Oil-GasAccumulation of Songliao Basin(in Chinese).Beijing:Petroleum Industry Press,2002:1-274.
[40]周建波,张兴洲,马志红等.中国东北地区的构造格局与盆地演化.石油与天然气地质,2009,30(5):530-538.Zhou J B,Zhang X Z,Ma Z H,et al.Tectonic frameworkand basin evolution in Northeast China.Oil&Gas Geology(in Chinese),2009,30(5):530-538.
[2]Jia D C,Hu R Z,Lu Y,et al.Collision belt between theKhanka block and the North China block in the YanbianRegion,Northeast China.Journal of Asian Earth Sciences,2004,23(2):211-219.
[3]Lin W,Faure M,Nomade S,et al.Permian-Triassic amalgamationof Asia:Insights from Northeast China sutures and their placein the final collision of North China and Siberia.ComptesRendus Geoscience,2008,340(2-3):190-201.
[4]任纪舜,姜春发,张正坤等.中国大地构造及其演化.北京:科学出版社,1980.Ren J S,Jiang C F,Zhang Z K,et al.The GeotectonicEvolution of China(in Chinese).Beijing:Science Press,1980.
[5]杨宝俊,刘财,梁铁成.满洲里-绥芬河地学断面域内莫霍的基本特征.长春科技大学学报,1998,28(1):111-113Yang B J,Liu C,Liang T C.The Basic Character of Moho inManzhouli-Suifenhe geoscience transecct.Journal of ChangchunUniversity of Science and Technology(in Chinese),1998,28(1):111-113.
[6]傅为洲,杨宝俊,刘财等.中国满洲里-绥芬河地学断面地震学研究.长春科技大学学报,1998,28(2):206-212Fu W Z,Yang B J,Liu C,et al.Study on the seismology inManzhouli-Suifenhe geoscience transect of China.Journal ofChangchun University of Science and Technology(in Chinese),1998,2:206-212.
[7]张凤旭,张兴洲,张凤琴等.中国东北地区重力场研究—利用改进的三方向小子域滤波划分主构造线及大地构造单元.地球物理学报,2010,53(6):1475-1485.Zhang F X,Zhang X Z,Zhang F Q,et al.Study of gravityfield in Northeastern China area:Classification of mainstructure lines and tectonic units using the improved three-directional small subdomain filtering.Chinese J.Geophys.(inChinese),2010,53(6):1475-1485.
[8]张凤旭,邰振华,张兴洲等.中国东北地区重力场研究----剩余重力场与重点油气勘探盆地的关系及油气勘探新领域.地球物理学进展,2011,26(2):424-432.Zhang F X,Tai Z H,Zhang X Z,et al.Study of gravity fieldin Northeastern China area:The relationship between residualgravity field and major exploratory basins,and new areas ofoil-gas exploration.Progress in Geophys.(in Chinese),2011,26(2):424-432.
[9]杜晓娟,孟令顺,张明仁.利用重力场研究东北地区断裂分布及构造分区.地球科学与环境学报,2009,31(2):200-206.Du X J,Meng L S,Zhang M R.Research on fault distributionand tectonic divisions in northeast China in terms of gravityfield.Journal of Earth Sciences and Environment(in Chinese),2009,31(2):200-206.
[10]胡旭芝,徐鸣洁,谢晓安等.中国东北地区航磁特征及居里面分析.地球物理学报,2006,49(6):1674-1681.Hu X Z,Xu M J,Xie X A,et al.A characteristic analysis ofaeromagnetic anomalies and Curie point isotherms in NortheastChina.Chinese J.Geophys.(in Chinese),2006,49(6):1674-1681.
[11]江为为,周立宏,肖敦清等.东北地区重磁场与地壳结构特征.地球物理学进展,2006,21(3):730-738.Jiang W W,Zhou L H,Xiao D Q,et al.The characteristicsof crust structure and the gravity and magnetic fields innortheast region of China.Progress in Geophysics(inChinese),2006,21(3):730-738.
[12]涂广红,江为为,朱东英等.中国东北地区剩余重磁异常特征与地质构造及成矿带的关系.地球物理学进展,2006,21(3):746-755Tu G H,Jiang W W,Zhu D Y,et al.The relationshipsbetween the characteristics of Northeast China residualgravity and magnetic anomalies and geological tectonic&metallogenic belt.Progress in Geophysics(in Chinese),2006,21(3):746-755.
[13]田有,刘财,冯晅.中国东北地区地壳、上地幔速度结构及其对矿产能源形成的控制作用.地球物理学报,2011,54(2):407-414Tian Y,Liu C,Feng X.P-wave velocity structure of crustand upper mantle in Northeast China and its control on theformation of mineral and energy.Chinese J.Geophys.(inChinese),2011,54(2):407-414
[14]刘财,张海江,杨宝俊等.小波变换在高分辨率地震勘探数据处理中的应用.长春地质学院学报,1996,26(1):78-82Liu C,Zhang H J,Yang B J,et al.Application of wavelettransform to digital processing in high resolution seismicprospecting.Journal of Changchun University of EarthSciences(in Chinese),1996,26(1):78-82
[15]Fedi M,Quarta T.Wavelet analysis for the regional-residualand local separation of potential field anomalies.Geophys.Prospecting,1998,46(5):507-525.
[16]Ucan O N,Seker S,Albora A M,et al.Separation of magneticfields in geophysical studies using a 2-D multi-resolutionWavelet analysis approach.Balkan Geophys.Soc.,2000,3(3):53-58.
[17]侯遵择,杨文采.中国重力异常的小波变换与多尺度分析.地球物理学报,1997,40(1):85-95。Hou Z Z,Yang W C.Wavelet transform and multi-scaleanalysis on gravity anomalies of China.Chinese J.Geophys.(in Chinese),1997,40(1):85-95.
[18]侯遵择,杨文采,刘家琦.中国大陆地壳密度差异多尺度反演.地球物理学报,1998,41(5):641-651.Hou Z Z,Yang W C,Liu J Q.Multiscale inversion of thedensity contrast within the crust of China.Chinese J.Geophys.(in Chinese),1998,41(5).641-651.
[19]高德章,侯遵择,唐建.东海及邻区重力异常多尺度分解.地球物理学报,2000,43(6):842-849。Gao D Z,Hou Z Z,Tang J.Multiscale analysis of gravityanomalies on east china sea and adjacent regions.Chinese J.Geophys.(in Chinese),2000,43(6):842-849.
[20]Albora A M,U?an O N.Gravity anomaly separation using2-D wavelet approach and average depth calculation.DogusUniv.J.(in Chinese),2001,3:1-12.
[21]邱宁,何展翔,昌彦君.分析研究基于小波分析与谱分析提高重力异常的分辨能力.地球物理学进展,2007,22(1):112-120.Qiu N,He Z X,Chang Y J.Ability of improving gravityanomaly resolution based on multiresolution wavelet analysisand power spectrum analysis.Prog.Geophys.(in Chinese),2007,22(1):112-20.
[22]Xu Y,Hao T Y,Li Z W,et al.Regional gravity anomalyseparation using wavelet transform and spectrum analysis.Journal of Geophysics and Engineering,2009,6(3):279-287.
[23]金旭,杨宝俊.中国满洲里-绥芬河地学断面地球物理场及深部构造特征研究.北京:地震出版社,1994.Jin X,Yang B J.Study on Geophysical and Deep TectonicCharacters in Manzhouli-Suifenhe Geoscience Transect ofChina(in Chinese).Beijing:Seismological PublishingHouse,1994.
[24]张萍,蒋秀琴.辽宁地区震源机制解及应力场特征的研究.东北地震研究,2000,16(1):1-7.Zhang P,Jiang X Q.Study of focal mechanism solutions andstress field characteristics in Liaoning region.SeismologicalResearch of Northeast China(in Chinese),2000,16(1):1-7.
[25]崔效锋,谢富仁,赵建涛.中国及邻区震源机制解的分区特征.地震地质,2005,27(2):298-307.Cui X F,Xie F R,Zhao J T.The regional characteristics offocal mechanism solutions in China and its adjacent areas.Seismology and Geology(in Chinese),2005,27(2):298-307.
[26]杨文采.地球物理反演的理论与方法.北京:地质出版社,1997.Yang W C.The Theory and Method of Geophysics Inversion(in Chinese).Beijing:Geology Publishing House,1997.
[27]Spector A,Grant F S.Statistical models for interpretingaeromagnetic data.Geophysics,1970,35(2):293-302.
[28]徐鸣洁,王良书,钟锴等.塔里木盆地重磁场特征与基底结构分析.高校地质学报,2005,11(4):585-592.Xu M J,Wang L S,Zhong K,et al.Features of gravitationaland magnetic fields in the Tarim basin and basement structureanalysis.Geological Journal of China Universities(inChinese),2005,11(4):585-592.
[29]杨宇山,李媛媛,刘天佑等.小波细节的微分特征及其在重力场断裂分析中的应用.地质与勘探,2003,39(1):41-44.Yang Y S,Li Y Y,Liu T Y,et al.The differentialcharacteristic of the wavelet details and its application in faultanalysis of gravity field.Geology and Prospecting(inChinese),2003,39(1):41-44.
[30]张先,赵丽,刘天佑等.北京地区航磁异常的多尺度分解及断裂研究.地震学报,2006,28(5):504-512.Zhang X,Zhao L,Liu T Y,et al.Multi-scale waveletseparation of aeromagnetic anomaly and study of faults inBeijing area.Acta Seismologica Sinica(in Chinese),2006,28(5):504-512.
[31]王桂梁,琚宜文,郑孟林等.中国北部能源盆地构造.徐州:中国矿业大学出版社,2007.Wang G L,Ju Y W,Zheng M L,et al.Tectonics of EnergyResource Basins in the Northern China(in Chinese).Xuzhou:China University of Mining and Technology Press,2007.
[32]叶慧文,张兴洲,周裕文.从蓝片岩及蛇绿岩特点看满洲里—绥芬河断面岩石圈结构与演化.//张兴洲.中国满洲里—绥芬河地学断面域内岩石圈结构及其演化的地质研究.北京:地震出版社,1994:73-83.Ye H W,Zhang X Z,Zhou Y W.Petrological structure andevolution of Manzhouli-Suifenhe section seeing fromcharacters of blueschist and ophiolite.//Zhang X Z ed.Study on Petrological Structure and Evolution Characters ofManzhouli-Suifenhe Section(in Chinese).Beijing:Seismological Publishing House,1994:73-83.
[33]李瑞山.新林蛇绿岩.黑龙江地质,1991,2(1):19-32.Li R S.Xinling Ophiolite.Heilongjiang Geology(inChinese),1991,2(1):19-32.
[34]张贻侠,孙运生,张兴洲等.中国满洲里—绥芬河地学断面1:1000000说明书.北京:地质出版社,1998:1-53.Zhang Y X,Sun Y S,Zhang X Z,et al.The 1:1000000Specification of the Manzhouli-Suifenhe Geo-transect(inChinese).Beijing:Geological Publishing House,1998:1-53.
[35]王跃,张兴洲,宋海峰等.牡丹江地区黑龙江杂岩的变质变形特征.吉林大学学报(地球科学版),2009,39(6):1066-1072.Wang Y,Zhang X Z,Song H F,et al.The metamorphic anddeformed characteristics of the Heilongjiang Melange inMudanjiang Area.Journal of Jilin University(Earth ScienceEdition)(in Chinese),2009,39(6):1066-1072.
[36]姚立珣,汪进,李亚荣.用震源机制解确定东北地区地壳应力场.东北地震研究,1992,8(2):27-32.Yao L X,Wang J,Li Y R.Crust stress in northeasternregion of China.Seismological Research of Northeast China(in Chinese),1992,8(2):27-32.
[37]葛荣峰,张庆龙,解国爱等.郯庐断裂带北段及邻区现代地震活动性与应力状态.地震地质,2009,31(1):141-154.Ge R F,Zhang Q L,Xie G A,et al.Seismic activity andstress state of the northern Tanlu Fault zone and its adjacentareas.Seismology and Geology(in Chinese),2009,31(1):141-154.
[38]张萍,孙文福,苗春兰等.东北地区中强地震震源机制解分析.地震地磁观测与研究,2009,30(1):12-19.Zhang P,Sun W F,Miao C L,et al.Analysis of focal-mechanism solution of moderately strong earthquakes inNortheast China.Seismological and Geomagnetic Observationand Research(in Chinese),2009,30(1):12-19.
[39]迟元林等著.松辽盆地深部结构及成盆动力学与油气聚集.北京:石油工业出版社,2002:1-274.Chi Y L,et al.Deep Structure,Basin Dynamics and Oil-GasAccumulation of Songliao Basin(in Chinese).Beijing:Petroleum Industry Press,2002:1-274.
[40]周建波,张兴洲,马志红等.中国东北地区的构造格局与盆地演化.石油与天然气地质,2009,30(5):530-538.Zhou J B,Zhang X Z,Ma Z H,et al.Tectonic frameworkand basin evolution in Northeast China.Oil&Gas Geology(in Chinese),2009,30(5):530-538.
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