川滇西部上新世以来构造地貌:断裂控制的盆地发育及对于远程陆内构造过程的约束
|
摘要
青藏高原隆升、周边地貌形成是新生代时期印度-欧亚板块碰撞后的重要响应。在滇西北地区发育了一系列由晚新生代(上新世以来)活动断裂所控制的盆地,例如宾川盆地、洱海盆地、鹤庆盆地、弥渡盆地等。宾川盆地是近南北向程海左行走滑断裂在走滑剪切作用下产生的北西向正断层和北东向走滑断层共同作用而形成的一个较大的拉分盆地。洱海盆地是由两组陡立的共轭张剪性(Transtensional)断层组限定的,为一伸展断陷盆地,总体上反映了近E-W向的区域伸展。滇西北地区发育的其它晚新生代盆地,如弥渡盆地、鹤庆盆地、剑川盆地等,也为区域走滑断裂及其分支断裂所控制,并且这些分支断裂在区域上为一组NE-SW和NW-SE向的共轭正断裂,反映了该区域近E-W向的伸展。将藏东南三江地区发育的活动断裂按照其走向分为三组:(1)NW-SE走向的断裂,如红河断裂、无量山-营盘山断裂等;(2)近N-S向断裂系,以程海断裂、小江断裂等为代表;(3)NE-SW走向的断裂,如丽江-剑川断裂、鹤庆-洱源断裂和南定河断裂等。这些断裂的震源机制解表明地震断裂活动性或者是走滑性质或者是伸展属性,它们的组合型式也揭示出藏东南三江地区在上新世以来表现为近E-W向的伸展。区域上,在藏东北部地区发育的断层构造组合普遍反映了以近E-W向挤压为主导的应力场。推测这一现象为上新世以来藏东地区上地壳围绕喜马拉雅东构造结做顺时针旋转所致,区域上受印度-欧亚会聚过程中印度板块顺时针旋转诱发的差异性应力场制约。
The uplift of Tibetan Plateau and the development of geomorphology in adjacent areas are the important response to the Cenozoic collision between Indian and Eurasian plates. There is a series of Late Cenozoic (since Pliocene) fault-bounded basins in northwestern Sichuan and Yunnan,e.g. Binchuan,Erhai,Heqing,Midu basins etc. Binchuan basin is of pull-apart origin bounded by normal faults in NW direction and strike-slip faults in NE direction in the N-S sinistral Chenghai strike-slip fault system. Erhai basin is an extensional rift basin delimited by two conjugate transtensional faults,suggesting an E-W extension. The other basins in northwestern Yunnan,such as Midu,Heqing,Jianchuan basins,were controlled by transtensional normal faults. Two branches of these faults in NE-SW and NW-SE direction form conjugate pairs,implying their origin by E-W extension. The active faults in the area are divided into three groups:(1) NW-SE trending faults,e.g. the Red River fault,Wuliangshan-Yingpanshan fault etc.; (2) N-S trending faults,e.g. Chenghai fault,Xiaojiang fault etc.; and (3) NE-SW trending faults,e.g. Lijiang-Jianchuan fault,Heqing-Eryuan fault,Nanting fault etc. From the focal mechanism solutions,these active faults possess strike-slipping or transextensional characteristics. Their association patterns reflect a regional extensional stress field in E-W direction in southeastern Tibet and Three River region since Pliocene. Regionally,the structural associations of active faults,in the northern part of the eastern Tibet,indicate the dominant role of an E-W compressional stress field. The overall stress field in eastern Tibet is possibly attributed to the clockwise rotation of the Tibetan crustal blocks around the eastern Himalayan syntaxis. The clockwise rotation of the Indian plate during its convergence with the Eurasian plate provide the plate scale driving force for the rotation of the Tibetan block.
The uplift of Tibetan Plateau and the development of geomorphology in adjacent areas are the important response to the Cenozoic collision between Indian and Eurasian plates. There is a series of Late Cenozoic (since Pliocene) fault-bounded basins in northwestern Sichuan and Yunnan,e.g. Binchuan,Erhai,Heqing,Midu basins etc. Binchuan basin is of pull-apart origin bounded by normal faults in NW direction and strike-slip faults in NE direction in the N-S sinistral Chenghai strike-slip fault system. Erhai basin is an extensional rift basin delimited by two conjugate transtensional faults,suggesting an E-W extension. The other basins in northwestern Yunnan,such as Midu,Heqing,Jianchuan basins,were controlled by transtensional normal faults. Two branches of these faults in NE-SW and NW-SE direction form conjugate pairs,implying their origin by E-W extension. The active faults in the area are divided into three groups:(1) NW-SE trending faults,e.g. the Red River fault,Wuliangshan-Yingpanshan fault etc.; (2) N-S trending faults,e.g. Chenghai fault,Xiaojiang fault etc.; and (3) NE-SW trending faults,e.g. Lijiang-Jianchuan fault,Heqing-Eryuan fault,Nanting fault etc. From the focal mechanism solutions,these active faults possess strike-slipping or transextensional characteristics. Their association patterns reflect a regional extensional stress field in E-W direction in southeastern Tibet and Three River region since Pliocene. Regionally,the structural associations of active faults,in the northern part of the eastern Tibet,indicate the dominant role of an E-W compressional stress field. The overall stress field in eastern Tibet is possibly attributed to the clockwise rotation of the Tibetan crustal blocks around the eastern Himalayan syntaxis. The clockwise rotation of the Indian plate during its convergence with the Eurasian plate provide the plate scale driving force for the rotation of the Tibetan block.
引文
[1]云南省地质矿产局.1991.大理幅(G-47-81-c)地质图(1:50000)
Allen CR,Gillespie AR,Han Y,Sieh Kand Zhang B and Zhu C.1984.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.GeologicalSociety of America Bulletin,95:686-700
Betrand G and Rangin C.2003.Tectonics of the western margin of theShan plateau(central Myanmar):Implication for the IndiaIndochina oblique convergence since the Oligocene.Journal of AsianEarth Sciences,21(10):1139-1157
Burchfiel BC and Wang EC.2003.Northwest-trending,middleCenozoic,left-lateral faults in southern Yunnan,China,and theirtectonic significance.Journal of Structural Geology,25(5):781-792
Bureau of Geology and Mineral Resource of Yunnan Province.1990.Regional Geology of Yunnan Province.Beijing:GeologicalPublishing House(in Chinese with English abstract)
Chen HH,Dobson J,Heller F and Hao J.1995.Paleomagnetic evidencefor clockwise rotation of the Simao region since the Cretaceous:Aconsequence of India-Asia collision.Earth and Planetary ScienceLetters,134(1-2):203-217
Chen WJ,Harrison FM and Lvera OM.1992.Thermochronology of theAilaoshan-Red River shear zone:A case study of multiple diffusiondomain model.Seismology and Geology,14(2):122-128(in Chinese with English abstract)
Chen Z,Burchfiel BC,Liu Y,King RW,Royden LH,Tang W,WangE,Zhao J and Zhang X.2000.Global positioning systemmeasurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation.Journal of GeophysicalResearch,105(B7):16215-16227
Cheng WZ,Yuan X and Zhang YJ.2006.Types of focal mechanismsolutions and parameter consistency of the sub-blocks in Sichuan andYunnan provinces.Acta Seismologica Sinica,28(6):561-573(in Chinese with English abstract)
Chung SL,Lo CH,Lee TY,Zhang YQ,Xie YW,Li XH,Wang KLandWang PL.1998.Diachronous uplift of the Tibetan plateau starting40Myr ago.Nature,394:769-773
Coleman M and Hodges K.1995.Evidence for Tibetan plateau upliftbefore14Myr ago from a new minimum age for east-west extension.Nature,374(6517):49-52
Deng QD,Zhang PZ,Ran YK,Yang XP,Min W and Chu QZ.2002.Basic characteristics of active tectonics of China.Science in China(Series D),32(12):1020-1030(in Chinese)
England P and Molnar P.1990.Right-lateral shear and rotation as theexplanation for strike-slip faulting in eastern Tibet.Nature,344(6262):140-142
Funahara S,Nishiwaki N,Miki M,Murata F,Otofuji Y and Wang YZ.1992.Paleomagnetic study of Cretaceous rocks from the YangzeBlock,central Yunnan,China:Implications for the India-Asiacollision.Earth and Planetary Science Letters,113(1-2):77-91
Funahara S,Nishiwaki N,Murata F,Otofuji Y and Wang YZ.1993.Clockwise rotation of the Red River fault inferred from paleomagneticstudy of Cretaceous rocks in the Shan-Thai-Malay Block of westernYunnan,China.Earth and Planetary Science Letters,117(1-2):29-42
Guo SM,Ji FJ,Xiang HF,Dong XQ,Yan FH,Zhang SL,Li XY andZhang WX.2001.Red River Active Fault Zone.Beijing:ChinaOcean Press,48-49(in Chinese with English abstract)
Harrison TM,Chen WJ and Leloup PH.1992.An Early Miocenetransition in deformation regime within the Red River fault zone,Yunnan,and its significance for Indo-Asian tectonics.Journal ofGeophysical Research,97(B5):7159-7182
Huang K and Opdyke ND.1993.Paleomagnetic results from Cretaceousand Jurassic rocks of South and Southwest Yunnan:Evidence forlarge clockwise rotations in the Indochina and Shan-Thai-Malayterranes.Earth and Planetary Science Letters,117(3-4):507-524
Institute of Geology,State Seismological Bureau,and SeismologicalBureau of Yunnan Province(IGCEA and SBYP).1990.ActiveFault in Northwest Yunnan Region.Beijing:Seismological Press(inChinese with English abstract)
Ji JQ,Zhong DLand Zhang LS.2000.Kinematics and dating of Cenozoicstrike-slip faults in the Tengchong area,West Yunnan:Implicationsfor the block movement in the southeastern Tibet Plateau.ScientiaGeologica Sinica,35(3):336-349(in Chinese with Englishabstract)
Khan MA,Treloar PJ,Searle MP and Jan MQ.2000.Tectonics of theNanga Parbat Syntaxis and the western Himalaya.Geological SocietySpecial Publication,London,170:485
Lee TY and Lawver LA.1994.Cenozoic plate reconstruction of the South China Sea region.Tectonophysics,235(1-2):149-180
Leloup PH,Harrison TM,Ryerson FJet al.1993.Structural,petrological and thermal evolution of a Tertiary ductile strike-slipshear zone,Diancang Shan,Yunnan.Journal of GeophysicalResearch,98:6715-6743
Leloup PH,Arnaud N,Lacassin R,Kienast JR,Harrison TM,Phan TT,Replumaz A and Tapponnier P.2001.New constraints on thestructure,thermochronology and timing of the Ailao Shan-Red Rivershear zone,SE Asia.Journal of Geophysical Research,66:1083-6732
Li YM,Xu HL,Sun JL,Qiu XL and Shi XB.2008.Characteristics offocal mechanism solutions of Red River Fault Zone and theirreflection on segmented fault activity.Journal of TropicalOceanography,27(2):32-39(in Chinese with English abstract)
Liu JL,Song ZJ,Cao SY,Zhai YF,Wang AJ,Gao L,Xiu QY and CaoDH.2006.The dynamic setting and processes of tectonic andmagmatic evolution of the oblique collision zone between Indian andEurasian plates:Exemplified by the tectonic evolution of the ThreeRiver region,eastern Tibet.Acta Petrologica Sinica,22(4):775-786(in Chinese with English abstract)
Liu JL,Cao SY,Zhai YF,Song ZJ,Wang,AJ,Xiu QY,Cao DH,GaoL and Guan H.2007.Rotation of crustal blocks as an explanation ofOligo-Miocene extension in southeastern Tibet:Evidenced by theDiancangshan and nearby metamorphic core complexes.EarthScience Frontiers,14(4):40-48(in Chinese with Englishabstract)
Liu PJ,Diao GL and Ning JY.2007.Fault plane solutions in Sichuan-Yunnan rhombic block and their dynamic implications.ActaSeismologica Sinica,29(5):449-458(in Chinese with Englishabstract)
Maluski H,Claude Lepvrier L and Jolivet A.2001.Ar-Ar and fission-track ages in the Song Chay Massif:Early Triassic and Cenozoictectonics in northern Vietnam.Journal of Asian Earth Sciences,19(1-2):233-248
Molnar P and Tapponnier P.1975.Cenozoic tectonics of Asia:Effects ofcontinental collision.Science,189:419-426
Morley CK.2002.A tectonic model for the Tertiary evolution of strikeslip faults and rift basins in SE Asia.Tectonophysics,347:189-215
Phan Thi KimVan.2006.The Lai Chau-Dien Bien Neotectonic fault zoneand its acting manifestations by moderate local earthquakes.Journalof Geology(Hanoi),Series B,27:30-39
Replumaz A,Lacassin R,Tapponnier P and Leloup PH.2001.Largeriver odd sets and Pliocene-Quaternary dextral slip rate on the RedRiver fault(Yunnan,China).Journal of Geophysical Research,106(B1):819-836
Sato K,Liu YY,Zhu ZC,Yang ZY and Otofuji Y.1999.Paleomagneticstudy of Middle Cretaceous rocks from Yunlong,western Yunnan,China:Evidence of southward displacement of Indochina.Earth andPlanetary Science Letters,165(1):1-15
Sato K,Liu YY,Zhu ZC,Yang ZY and Otofuji Y.2001.Tertiarypaleomagnetic data from northwestern Yunnan,China:Furtherevidence for large clockwise rotation of the Indochina block and itstectonic implications.Earth and Planetary Science Letters,185(1-2):185-198
Scharer U,Tapponnier P,Lacassin R,Leloup PH,Zhong DLand Ji SC. 1990.Intraplate tectonics in Asia:A precise age for large-scaleMiocene movement along the Ailao Shan-Red River shear zone,China.Earth and Planetary Science Letters,97(1-2):65-77
Scharer U,Zhang LS and Tapponnier P.1994.Duration of strike-slipmovements in large shear zones:The Red River belt,China.Earthand Planetary Science Letters,126(4):379-397
Schoenbohm LM,Burchfiel BC,Chen LZ and Yin JY.2006.Miocene topresent activity along the Red River fault,China,in the context ofcontinental extrusion,upper crustal rotation,and lower crustal flow.Geological Society of America Bulletin,118(5-6):672-688
Socquet A and Pubellier M.2005.Cenozoic deformation in westernYunnan(China-Myanmar border).Journal of Asian Earth Sciences,24(4):495-515
Song FM,Wang YP,Shen J,Cao ZQ and Shen XH.1997.Thedevelopment stages of the basins along the middle segment of theXiaojiang fault zone and its relation to regional tectonic movement.Seismology and Geology,19(3):211-217(in Chinese withEnglish abstract)
Sun Z,Zhong ZH,Zhou D,Qiu XL and Wu SM.2003.Deformationmechanism of Red River fault zone during Cenozoic and experimentalevidences related to Yinggehai basin formation.Journal of TropicalOceanography,22(2):1-9(in Chinese with English abstract)
Tan XH.1999.Characteristics and formation mechanism of Cenozoicstructural basins in the Three River area of west Yunnan.YunnanGeology,18(2):112-121(in Chinese with English abstract)
Tang Y,Liu JL,Tran MD and Song ZJ.2009.Structural characteristics,remote sensing interpretation of the Dien Bien Phu strike slip faultzone and regional tectonic implication.Acta Geologica Sinica,83(10):1401-1414(in Chinese with English abstract)
Tapponnier P,Lacassin R,Leloup PH,Scharer U,Zhong DL,Liu XH,Ji SC,Zhang LS and Zhong JY.1990.The Ailao Shan/Red Rivermetamorphic belt:Tertiary left-lateral shear between Indo-China andSouth China.Nature,343:431-437
The Earthquake Disaster Prevention Department of the State SeismologicalBureau.1995.Catalogue of Chinese Historical Strong Earthquakes.Beijing:Seismological Press(in Chinese with English abstract)
The Earthquake Disaster Prevention Department of the State SeismologicalBureau.1999.Catalogue of Later Day Earthquake.Beijing:ChinaScience and Technology Press(in Chinese with English abstract)
Turner S,Hawkesworth C and Liu JQ.1993.Timing of Tibet upliftconstrained by analysis of volcanic rocks.Nature,364(6432):50-54
Zhang LS and Zhong DL.1996.The Red River strike-slip shear zone andCenozoic tectonics of East Asia continent.Chinese Journal ofGeology,31(4):327-341(in Chinese with English abstract)
Zhang LS and Scharer U.1999.Age and origin of magmatism along theCenozoic Red River shear belt,China.Contributions to Mineralogyand Petrology,134(1):67-85
Zhang PZ,Deng QD,Zhang GM,Ma J,Gan WJ,Min W,Mao FY andWang Q.2003.Active tectonic blocks and strong earthquakes in thecontinent of China.Science in China(Series D),33(Suppl.):12-20(in Chinese with English abstract)
Zhang PZ,Shen ZK,Wang M,Gan WJ,Burgmann R,Molnar P,WangQ,Niu ZJ,Sun JZ,Wu JC,Sun HR and You XZ.2004.Continuous deformation of the Tibetan Plateau from global positioningsystem data.Geology,32:809-812
陈文寄,Harrison FM,Lvera OM.1992.哀牢山-红河剪切带的热年代学研究.地震地质,14(2):122-128
程万正,阮祥,张永久.2006.川滇次级地块震源机制解类型与一致性参数.地震学报,28(6):561-573
邓起东,张培震,冉勇康,杨晓平,闵伟,楚全芝.2002.中国活动构造基本特征.中国科学(D辑),32(12):1020-1030
国家地震局地质研究所,云南省地震局.1990.滇西北地区活动断裂.北京:地震出版社,112-113
国家地震局震害防御司.1995.中国历史强震目录.北京:地震出版社
虢顺民,计凤桔,向宏发,董兴权,严富华,张双林,李新元,张晚霞.2001.红河活动断裂带.北京:海洋出版社,48-49
季建清,钟大赉,张连生.2000.滇西南新生代走滑断裂运动学、年代学及对青藏高原东南部块体运动学的意义.地质科学,35(3):336-349
李亚敏,徐辉龙,孙金龙,丘学林,施小斌.2008.红河断裂带及其邻区的震源机制解特征及其反映的断裂活动分段性.热带海洋学报,27(2):32-39
刘俊来,宋志杰,曹淑云,翟云峰,王安建,高兰,修群业,曹殿华.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程———以藏东三江地区构造演化为例.岩石学报,22(4):775-786
刘俊来,曹淑云,翟云峰,宋志杰,王安建,修群业,曹殿华,高兰,管烨.2007.用陆块旋转解释藏东南渐新世-中新世伸展作用———来自点苍山及邻区变质核杂岩的证据.地学前缘,14(4):40-48
刘平江,刁桂苓,宁杰远.2007.川滇地块的震源机制解特征及其地球动力学解释.地震学报,29(5):449-458
宋方敏,汪一鹏,沈军等.1997.小江断裂带中段盆地的发育阶段及其与区域构造运动的关系.地震地质,19(3):211-217
孙珍,钟志洪,周蒂,丘学林,吴世敏.2003.红河断裂带的新生代变形机制及莺歌海盆地的实验证据.热带海洋学报,22(2):1-9
谭筱虹.1999.滇西三江地区新生代构造盆地的特征及形成机制.云南地质,18(2):112-121
唐渊,刘俊来,Tran My Dung,宋志杰.2009.奠边府走滑断裂带的构造特征、遥感解译及其区域构造意义.地质学报,83(10):1401-1414
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社,558-559
张连生,钟大赉.1996.从红河剪切带走滑运动看东亚大陆新生代构造.地质科学,31(4):327-341
张培震,邓起东,张国民,马瑾,甘卫军,闵伟,毛凤英,王琪.2003.中国大陆的强震活动与活动地块.中国科学(D辑),33(增刊):12-20
中国地震局震害防御司.1999.中国近代地震目录.北京:中国科学技术出版社
Allen CR,Gillespie AR,Han Y,Sieh Kand Zhang B and Zhu C.1984.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.GeologicalSociety of America Bulletin,95:686-700
Betrand G and Rangin C.2003.Tectonics of the western margin of theShan plateau(central Myanmar):Implication for the IndiaIndochina oblique convergence since the Oligocene.Journal of AsianEarth Sciences,21(10):1139-1157
Burchfiel BC and Wang EC.2003.Northwest-trending,middleCenozoic,left-lateral faults in southern Yunnan,China,and theirtectonic significance.Journal of Structural Geology,25(5):781-792
Bureau of Geology and Mineral Resource of Yunnan Province.1990.Regional Geology of Yunnan Province.Beijing:GeologicalPublishing House(in Chinese with English abstract)
Chen HH,Dobson J,Heller F and Hao J.1995.Paleomagnetic evidencefor clockwise rotation of the Simao region since the Cretaceous:Aconsequence of India-Asia collision.Earth and Planetary ScienceLetters,134(1-2):203-217
Chen WJ,Harrison FM and Lvera OM.1992.Thermochronology of theAilaoshan-Red River shear zone:A case study of multiple diffusiondomain model.Seismology and Geology,14(2):122-128(in Chinese with English abstract)
Chen Z,Burchfiel BC,Liu Y,King RW,Royden LH,Tang W,WangE,Zhao J and Zhang X.2000.Global positioning systemmeasurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation.Journal of GeophysicalResearch,105(B7):16215-16227
Cheng WZ,Yuan X and Zhang YJ.2006.Types of focal mechanismsolutions and parameter consistency of the sub-blocks in Sichuan andYunnan provinces.Acta Seismologica Sinica,28(6):561-573(in Chinese with English abstract)
Chung SL,Lo CH,Lee TY,Zhang YQ,Xie YW,Li XH,Wang KLandWang PL.1998.Diachronous uplift of the Tibetan plateau starting40Myr ago.Nature,394:769-773
Coleman M and Hodges K.1995.Evidence for Tibetan plateau upliftbefore14Myr ago from a new minimum age for east-west extension.Nature,374(6517):49-52
Deng QD,Zhang PZ,Ran YK,Yang XP,Min W and Chu QZ.2002.Basic characteristics of active tectonics of China.Science in China(Series D),32(12):1020-1030(in Chinese)
England P and Molnar P.1990.Right-lateral shear and rotation as theexplanation for strike-slip faulting in eastern Tibet.Nature,344(6262):140-142
Funahara S,Nishiwaki N,Miki M,Murata F,Otofuji Y and Wang YZ.1992.Paleomagnetic study of Cretaceous rocks from the YangzeBlock,central Yunnan,China:Implications for the India-Asiacollision.Earth and Planetary Science Letters,113(1-2):77-91
Funahara S,Nishiwaki N,Murata F,Otofuji Y and Wang YZ.1993.Clockwise rotation of the Red River fault inferred from paleomagneticstudy of Cretaceous rocks in the Shan-Thai-Malay Block of westernYunnan,China.Earth and Planetary Science Letters,117(1-2):29-42
Guo SM,Ji FJ,Xiang HF,Dong XQ,Yan FH,Zhang SL,Li XY andZhang WX.2001.Red River Active Fault Zone.Beijing:ChinaOcean Press,48-49(in Chinese with English abstract)
Harrison TM,Chen WJ and Leloup PH.1992.An Early Miocenetransition in deformation regime within the Red River fault zone,Yunnan,and its significance for Indo-Asian tectonics.Journal ofGeophysical Research,97(B5):7159-7182
Huang K and Opdyke ND.1993.Paleomagnetic results from Cretaceousand Jurassic rocks of South and Southwest Yunnan:Evidence forlarge clockwise rotations in the Indochina and Shan-Thai-Malayterranes.Earth and Planetary Science Letters,117(3-4):507-524
Institute of Geology,State Seismological Bureau,and SeismologicalBureau of Yunnan Province(IGCEA and SBYP).1990.ActiveFault in Northwest Yunnan Region.Beijing:Seismological Press(inChinese with English abstract)
Ji JQ,Zhong DLand Zhang LS.2000.Kinematics and dating of Cenozoicstrike-slip faults in the Tengchong area,West Yunnan:Implicationsfor the block movement in the southeastern Tibet Plateau.ScientiaGeologica Sinica,35(3):336-349(in Chinese with Englishabstract)
Khan MA,Treloar PJ,Searle MP and Jan MQ.2000.Tectonics of theNanga Parbat Syntaxis and the western Himalaya.Geological SocietySpecial Publication,London,170:485
Lee TY and Lawver LA.1994.Cenozoic plate reconstruction of the South China Sea region.Tectonophysics,235(1-2):149-180
Leloup PH,Harrison TM,Ryerson FJet al.1993.Structural,petrological and thermal evolution of a Tertiary ductile strike-slipshear zone,Diancang Shan,Yunnan.Journal of GeophysicalResearch,98:6715-6743
Leloup PH,Arnaud N,Lacassin R,Kienast JR,Harrison TM,Phan TT,Replumaz A and Tapponnier P.2001.New constraints on thestructure,thermochronology and timing of the Ailao Shan-Red Rivershear zone,SE Asia.Journal of Geophysical Research,66:1083-6732
Li YM,Xu HL,Sun JL,Qiu XL and Shi XB.2008.Characteristics offocal mechanism solutions of Red River Fault Zone and theirreflection on segmented fault activity.Journal of TropicalOceanography,27(2):32-39(in Chinese with English abstract)
Liu JL,Song ZJ,Cao SY,Zhai YF,Wang AJ,Gao L,Xiu QY and CaoDH.2006.The dynamic setting and processes of tectonic andmagmatic evolution of the oblique collision zone between Indian andEurasian plates:Exemplified by the tectonic evolution of the ThreeRiver region,eastern Tibet.Acta Petrologica Sinica,22(4):775-786(in Chinese with English abstract)
Liu JL,Cao SY,Zhai YF,Song ZJ,Wang,AJ,Xiu QY,Cao DH,GaoL and Guan H.2007.Rotation of crustal blocks as an explanation ofOligo-Miocene extension in southeastern Tibet:Evidenced by theDiancangshan and nearby metamorphic core complexes.EarthScience Frontiers,14(4):40-48(in Chinese with Englishabstract)
Liu PJ,Diao GL and Ning JY.2007.Fault plane solutions in Sichuan-Yunnan rhombic block and their dynamic implications.ActaSeismologica Sinica,29(5):449-458(in Chinese with Englishabstract)
Maluski H,Claude Lepvrier L and Jolivet A.2001.Ar-Ar and fission-track ages in the Song Chay Massif:Early Triassic and Cenozoictectonics in northern Vietnam.Journal of Asian Earth Sciences,19(1-2):233-248
Molnar P and Tapponnier P.1975.Cenozoic tectonics of Asia:Effects ofcontinental collision.Science,189:419-426
Morley CK.2002.A tectonic model for the Tertiary evolution of strikeslip faults and rift basins in SE Asia.Tectonophysics,347:189-215
Phan Thi KimVan.2006.The Lai Chau-Dien Bien Neotectonic fault zoneand its acting manifestations by moderate local earthquakes.Journalof Geology(Hanoi),Series B,27:30-39
Replumaz A,Lacassin R,Tapponnier P and Leloup PH.2001.Largeriver odd sets and Pliocene-Quaternary dextral slip rate on the RedRiver fault(Yunnan,China).Journal of Geophysical Research,106(B1):819-836
Sato K,Liu YY,Zhu ZC,Yang ZY and Otofuji Y.1999.Paleomagneticstudy of Middle Cretaceous rocks from Yunlong,western Yunnan,China:Evidence of southward displacement of Indochina.Earth andPlanetary Science Letters,165(1):1-15
Sato K,Liu YY,Zhu ZC,Yang ZY and Otofuji Y.2001.Tertiarypaleomagnetic data from northwestern Yunnan,China:Furtherevidence for large clockwise rotation of the Indochina block and itstectonic implications.Earth and Planetary Science Letters,185(1-2):185-198
Scharer U,Tapponnier P,Lacassin R,Leloup PH,Zhong DLand Ji SC. 1990.Intraplate tectonics in Asia:A precise age for large-scaleMiocene movement along the Ailao Shan-Red River shear zone,China.Earth and Planetary Science Letters,97(1-2):65-77
Scharer U,Zhang LS and Tapponnier P.1994.Duration of strike-slipmovements in large shear zones:The Red River belt,China.Earthand Planetary Science Letters,126(4):379-397
Schoenbohm LM,Burchfiel BC,Chen LZ and Yin JY.2006.Miocene topresent activity along the Red River fault,China,in the context ofcontinental extrusion,upper crustal rotation,and lower crustal flow.Geological Society of America Bulletin,118(5-6):672-688
Socquet A and Pubellier M.2005.Cenozoic deformation in westernYunnan(China-Myanmar border).Journal of Asian Earth Sciences,24(4):495-515
Song FM,Wang YP,Shen J,Cao ZQ and Shen XH.1997.Thedevelopment stages of the basins along the middle segment of theXiaojiang fault zone and its relation to regional tectonic movement.Seismology and Geology,19(3):211-217(in Chinese withEnglish abstract)
Sun Z,Zhong ZH,Zhou D,Qiu XL and Wu SM.2003.Deformationmechanism of Red River fault zone during Cenozoic and experimentalevidences related to Yinggehai basin formation.Journal of TropicalOceanography,22(2):1-9(in Chinese with English abstract)
Tan XH.1999.Characteristics and formation mechanism of Cenozoicstructural basins in the Three River area of west Yunnan.YunnanGeology,18(2):112-121(in Chinese with English abstract)
Tang Y,Liu JL,Tran MD and Song ZJ.2009.Structural characteristics,remote sensing interpretation of the Dien Bien Phu strike slip faultzone and regional tectonic implication.Acta Geologica Sinica,83(10):1401-1414(in Chinese with English abstract)
Tapponnier P,Lacassin R,Leloup PH,Scharer U,Zhong DL,Liu XH,Ji SC,Zhang LS and Zhong JY.1990.The Ailao Shan/Red Rivermetamorphic belt:Tertiary left-lateral shear between Indo-China andSouth China.Nature,343:431-437
The Earthquake Disaster Prevention Department of the State SeismologicalBureau.1995.Catalogue of Chinese Historical Strong Earthquakes.Beijing:Seismological Press(in Chinese with English abstract)
The Earthquake Disaster Prevention Department of the State SeismologicalBureau.1999.Catalogue of Later Day Earthquake.Beijing:ChinaScience and Technology Press(in Chinese with English abstract)
Turner S,Hawkesworth C and Liu JQ.1993.Timing of Tibet upliftconstrained by analysis of volcanic rocks.Nature,364(6432):50-54
Zhang LS and Zhong DL.1996.The Red River strike-slip shear zone andCenozoic tectonics of East Asia continent.Chinese Journal ofGeology,31(4):327-341(in Chinese with English abstract)
Zhang LS and Scharer U.1999.Age and origin of magmatism along theCenozoic Red River shear belt,China.Contributions to Mineralogyand Petrology,134(1):67-85
Zhang PZ,Deng QD,Zhang GM,Ma J,Gan WJ,Min W,Mao FY andWang Q.2003.Active tectonic blocks and strong earthquakes in thecontinent of China.Science in China(Series D),33(Suppl.):12-20(in Chinese with English abstract)
Zhang PZ,Shen ZK,Wang M,Gan WJ,Burgmann R,Molnar P,WangQ,Niu ZJ,Sun JZ,Wu JC,Sun HR and You XZ.2004.Continuous deformation of the Tibetan Plateau from global positioningsystem data.Geology,32:809-812
陈文寄,Harrison FM,Lvera OM.1992.哀牢山-红河剪切带的热年代学研究.地震地质,14(2):122-128
程万正,阮祥,张永久.2006.川滇次级地块震源机制解类型与一致性参数.地震学报,28(6):561-573
邓起东,张培震,冉勇康,杨晓平,闵伟,楚全芝.2002.中国活动构造基本特征.中国科学(D辑),32(12):1020-1030
国家地震局地质研究所,云南省地震局.1990.滇西北地区活动断裂.北京:地震出版社,112-113
国家地震局震害防御司.1995.中国历史强震目录.北京:地震出版社
虢顺民,计凤桔,向宏发,董兴权,严富华,张双林,李新元,张晚霞.2001.红河活动断裂带.北京:海洋出版社,48-49
季建清,钟大赉,张连生.2000.滇西南新生代走滑断裂运动学、年代学及对青藏高原东南部块体运动学的意义.地质科学,35(3):336-349
李亚敏,徐辉龙,孙金龙,丘学林,施小斌.2008.红河断裂带及其邻区的震源机制解特征及其反映的断裂活动分段性.热带海洋学报,27(2):32-39
刘俊来,宋志杰,曹淑云,翟云峰,王安建,高兰,修群业,曹殿华.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程———以藏东三江地区构造演化为例.岩石学报,22(4):775-786
刘俊来,曹淑云,翟云峰,宋志杰,王安建,修群业,曹殿华,高兰,管烨.2007.用陆块旋转解释藏东南渐新世-中新世伸展作用———来自点苍山及邻区变质核杂岩的证据.地学前缘,14(4):40-48
刘平江,刁桂苓,宁杰远.2007.川滇地块的震源机制解特征及其地球动力学解释.地震学报,29(5):449-458
宋方敏,汪一鹏,沈军等.1997.小江断裂带中段盆地的发育阶段及其与区域构造运动的关系.地震地质,19(3):211-217
孙珍,钟志洪,周蒂,丘学林,吴世敏.2003.红河断裂带的新生代变形机制及莺歌海盆地的实验证据.热带海洋学报,22(2):1-9
谭筱虹.1999.滇西三江地区新生代构造盆地的特征及形成机制.云南地质,18(2):112-121
唐渊,刘俊来,Tran My Dung,宋志杰.2009.奠边府走滑断裂带的构造特征、遥感解译及其区域构造意义.地质学报,83(10):1401-1414
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社,558-559
张连生,钟大赉.1996.从红河剪切带走滑运动看东亚大陆新生代构造.地质科学,31(4):327-341
张培震,邓起东,张国民,马瑾,甘卫军,闵伟,毛凤英,王琪.2003.中国大陆的强震活动与活动地块.中国科学(D辑),33(增刊):12-20
中国地震局震害防御司.1999.中国近代地震目录.北京:中国科学技术出版社
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