红河断裂带活动性研究
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摘要
红河断裂带是一条大型的走滑断裂带,该断裂带北起青藏高原东部,云南西北部,穿越越南北部,向东南延伸到南海,全长超过1000km。根据印支半岛前新生代的古地块与华南地块的接触关系,将红河断裂带分为海陆两段。断裂带自从第三纪以来,经历了左旋运动,右旋运动以及局部旋转,南北两段的活动性有一定的差异性,现今断裂带在最北端活动强烈,曾多次发生6级以上地震,南段现今活动较为平静。
The Red River Fault Zone is a gigantic sliding fault zone beginning from the east of Qinzang plateau in the north to the northwest of Yunnan, and passing through the north of Vietnam, and then extending to South China Sea, the whole length is over 1000km. Based on the contacted relationship between the old pre-Cenozoic massif in Indochina Peninsula and the South China massif, the Red River Fault Zone was divided into two parts extending from land to ocean, north and south segments. Since the Tertiary period, the Red River Fault Zone suffered the sinistral movement, dextral movement and local rotation. The activities of the north and the south segments were different. The activities of the north segment were violent at the end of the north in modern time where many earthquakes M≥60 occurred, today the activities of the south segment are calmer.
The Red River Fault Zone is a gigantic sliding fault zone beginning from the east of Qinzang plateau in the north to the northwest of Yunnan, and passing through the north of Vietnam, and then extending to South China Sea, the whole length is over 1000km. Based on the contacted relationship between the old pre-Cenozoic massif in Indochina Peninsula and the South China massif, the Red River Fault Zone was divided into two parts extending from land to ocean, north and south segments. Since the Tertiary period, the Red River Fault Zone suffered the sinistral movement, dextral movement and local rotation. The activities of the north and the south segments were different. The activities of the north segment were violent at the end of the north in modern time where many earthquakes M≥60 occurred, today the activities of the south segment are calmer.
引文
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[25] 何丽娟,熊亮萍,汪集杨,等.莺歌海盆地构造热演化模拟研究[J].中国科学(D辑),2000,30(4):415-419.
[26] 詹文欢,朱俊江,孙宗勋,等.南海西北部壳体新构造运动及其演化模式[J].大地构造与成矿学,2001,25(4):353-360.
[27] 朱俊江,詹文欢,唐 诚,等.水系的分形特征与红河断裂带的活动性关系初探[J].华南地震,2002,22(1);1-7.
[28] 计凤桔,李兴元,虢顺民,等.红河断裂弥渡—大马街区段的几何结构及其活动性研究[A].国家地震局地质研究所,活动断裂研究(2)[C].北京:地震出版社,1992,73-84.
[29] 向宏发,严富华,张双林,等.红河断裂带戛洒—东峨段水系发育与断裂位错分布的研究[A].国家地震局地质研究所,活动断裂研究(3)[C].北京:地震出版社,1994,93-103.
[30] 万 玲,吴能友.红河断裂带在南海海域的延伸[A].中国地球物理年会2001年年刊[C].2001.
[31] 任纪舜,金小赤.红河断裂的新观察[J].地质论评,1996,42(5):439-442.
[32] HuchonP,LePichonX,RanginC.IndochinaPeninsulaandthecollisionofIndiaandEurasi
[2] 郭令智,钟志洪,王良书,等.莺歌海盆地周边区域构造演化[J].高校地质学报,2001,7(1):1-12.
[3] 张进江,钟大赉,周 勇.东南亚及哀牢山红河构造带构造演化的讨论[J].地质论评,1999,45(4):337-343.
[4] TapponnierP,LacassinR,LeloupPH,etal.TheAilaoShan/RedRivermetamorphicbelt:TertiaryLeft-LateralshearbetweenIndochinaandSouthChins[J].Nature,1990,343:431-437.
[5] LeloupHP,LacassinR,TapponnierP,etc.TheAilaoShan-RedRivershearzone(Yunnan,China),TertiarytransformboundaryofIndochina[J].Tectonophysics,1995,251:3-84.
[6] WangJianghai,AnYin,T.MarkHarrision,etc.AtectonicmodelforCenzoicigneousactivitiesintheeasternIndo-Asiancollisionzone[J].EarthPlanet.Sci.Lett,2001,188:123-133.
[7] Sch rerU,TapponnierP,LacassinR,etal.IntraplatetectonicsinAsia:apreciseageofforlarge-scaleMiocenemovenmentalongtheAilaoShan-RedRivershearzone,China[J].EarthPlanet.Sci.Lett,1990,97:65-77.
[8] Sch rerU,ZhangLiansheng,TapponnierP.Durationofstrike-slipmovementinlargeshearzones:TheRedRiverbelt,China[J].EarthPlanet.Sci.Lett,1994,126:379-397.
[9] HarrissonTM,ChengW,LeloupHP,etal.AnearlyMiocenceTransitionindeformationregimwithintheRedRiverfaultzone,Yunnan,anditssignificanceforIndo-Asiantectonic[J].Journalgeophysicsresearch,1992,97:7159-7182.
[10] 陈文寄,哈里森TM,洛费拉OM.哀牢山—红河剪切带的热年代学研究—多重扩散域模式的应用实例[J].地震地质,1992,14(2):121-128.
[11] 万京林,李 齐,陈文寄.哀牢山—红河左旋走滑剪切带构造抬升时间序列的裂变径迹证据[J].地震地质,1997,19(1):87-90.
[12] 艾伦CR,韩源,西KR,等.红河断裂带的第四纪活动研究—现代活动概貌和活动断裂证据[J].地震研究,1984,7(1):39-51.
[13] 艾伦CR,韩 源,西KR,等.红河断裂带的第四纪活动研究—断裂活动特征、走滑速率与地震重复周期探讨[J].地震研究,1984,7(2):171-185.
[14] RanginC,KleinM,RoquesD,etal.TheRedRiverfaultsystemintheTonkinGulf,Vietnam[J].Tectonophysics,1995,243(3-4):209-222.
[15] FunaharaS,NishiwakiN,MurataF,etal.ClockwiserotationoftheRedRiverfaultinferredfrompaleomagneticstudyofCretaceousrocksintheShan-Thai-MalayblockofwesternYunnan,China[J].EarthPlatnet.Sci.Lett,1993,117:29-42.
[16] ChengHaihong,DobsonJ,HellerF,etal.PaleomagneticevidenceforclockwiserotationoftheSimaoregionsincetheCretaceous:AconsequenceofIndia-Asiacollision[J].EarthPlanet.Sci.Lett,1995,134:203-217.
[17] HuangKainian,NeilD,Opdyke.PaleomagneticresultsfromCretaceousandJurassicrocksofSouthandSoutheastYunnan:evidenceforlargeclockwiserotationsintheIndochinaandShan-Thai-Malayterranes[J].EarthPlanet.Sci.Lett,1993,117:507-524.
[18] Chung,SL,Lee,etal.IntraplateextensionpriortocontinentalextensionalongtheAilaoShan-RdeRivershearzone[J].Geology,25:311-314.
[19] JolivetL,MaluskiH,BeyssacO,etal.Oligocene-MioceneBuKhangextensionalgneissdomeinVietnam:Geodynamicimplications[J].Geology,1999,27:67-70.
[20] 刘以宣.南海新构造与地壳稳定性[M].北京:科学出版社,1994.
[21] 计凤桔,虢顺民,向宏发.红河断裂带第四纪活动的时空演化特征[J].地震地质,1997,19(2):108-114.
[22] 龚再升,李思田,等.南海北部大陆边缘盆地分析与油气聚集[M].科学出版社,1997.
[23] 丁中一,杨小毛,马莉,等.莺歌海盆地拉张性质的研究[J].地球物理学报,1999,42(1):53-61.
[24] 孙家振,李兰斌,杨士恭,等.转换—伸展盆地—莺歌海的演化[J].地球科学,1995,20(3):243-249.
[25] 何丽娟,熊亮萍,汪集杨,等.莺歌海盆地构造热演化模拟研究[J].中国科学(D辑),2000,30(4):415-419.
[26] 詹文欢,朱俊江,孙宗勋,等.南海西北部壳体新构造运动及其演化模式[J].大地构造与成矿学,2001,25(4):353-360.
[27] 朱俊江,詹文欢,唐 诚,等.水系的分形特征与红河断裂带的活动性关系初探[J].华南地震,2002,22(1);1-7.
[28] 计凤桔,李兴元,虢顺民,等.红河断裂弥渡—大马街区段的几何结构及其活动性研究[A].国家地震局地质研究所,活动断裂研究(2)[C].北京:地震出版社,1992,73-84.
[29] 向宏发,严富华,张双林,等.红河断裂带戛洒—东峨段水系发育与断裂位错分布的研究[A].国家地震局地质研究所,活动断裂研究(3)[C].北京:地震出版社,1994,93-103.
[30] 万 玲,吴能友.红河断裂带在南海海域的延伸[A].中国地球物理年会2001年年刊[C].2001.
[31] 任纪舜,金小赤.红河断裂的新观察[J].地质论评,1996,42(5):439-442.
[32] HuchonP,LePichonX,RanginC.IndochinaPeninsulaandthecollisionofIndiaandEurasi
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