红河断裂带莺歌海段地质构造特征
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摘要
红河入海后的地质构造特征研究是当前红河断裂带研究的薄弱环节。结合莺歌海地区重力和地震资料解释与前人研究成果,系统总结了红河断裂带莺歌海盆地内的几何学、运动学特征,并根据莺歌海盆地沉积中心迁移规律获得了红河断裂带的年代学数据。研究认为:红河断裂带在入海口附近分叉,其中Tien Lang断层折向NE,呈马尾状展布;在莺歌海盆地内红河断裂带分支为A(I号断层)、B、C和D(莺西断层)4条断层,其中A断层是最主要的一条分支断层。莺歌海盆地内的分支断层均呈近NW—SE走向,延伸420～500km,其地震解释剖面上发育的典型花状构造和马尾状Tien Lang断层共同指示该断层具有走滑运动性质;红河断裂带对莺歌海盆地的沉积具有明显的控制作用,盆地沉积中心变化规律揭示红河断裂带在30～15.5Ma期间具有左行走滑运动性质,15.5～5.5Ma期间为左行向右行转换阶段,发生了强烈的构造反转作用,5.5Ma以来具有右行走滑运动特征。
The geological structure characteristic of Red River fault zone after entering South China Sea is one bottleneck in research. Based on the geometry and kinematics features of Red River fault zone among the Yinggehai area and tectonic interpretation of aerial gravity anomaly and seismic profiles, this study obtained the chronological data of Red River fault zone combined with the depocenter migration regulation of Yinggehai Basin. The Red River fault zone divaricates nearby the entrance of South China Sea. The The Tien Lang fault, one of the branches, converts into NE direction with the horsetail form. The Red River fault zone divaricates into four branches among the Yinggehai Basin, here named A(No.I Fault), B, C and D(Ying Xi Fault). All of these 4 branches strike into NW—SE with the extension length ranging from 420 to 500 km. The typical flower structure in the seismic profiles and the horsetail form of Tien Lang fault jointly indicate that the Red River fault zone is characterized by strike-slip movement. The Red River fault zone controls sedimentation of Yinggehai Basin. Change regulation of depocenter migration of the Yinggehai basin reveals that the fault was sinistral strike-slip during 30～15.5 Ma, transformed to dextral strike-slip during 15.5～5.5Ma, and resumed to dextral strike-slip since 5.5Ma.
The geological structure characteristic of Red River fault zone after entering South China Sea is one bottleneck in research. Based on the geometry and kinematics features of Red River fault zone among the Yinggehai area and tectonic interpretation of aerial gravity anomaly and seismic profiles, this study obtained the chronological data of Red River fault zone combined with the depocenter migration regulation of Yinggehai Basin. The Red River fault zone divaricates nearby the entrance of South China Sea. The The Tien Lang fault, one of the branches, converts into NE direction with the horsetail form. The Red River fault zone divaricates into four branches among the Yinggehai Basin, here named A(No.I Fault), B, C and D(Ying Xi Fault). All of these 4 branches strike into NW—SE with the extension length ranging from 420 to 500 km. The typical flower structure in the seismic profiles and the horsetail form of Tien Lang fault jointly indicate that the Red River fault zone is characterized by strike-slip movement. The Red River fault zone controls sedimentation of Yinggehai Basin. Change regulation of depocenter migration of the Yinggehai basin reveals that the fault was sinistral strike-slip during 30～15.5 Ma, transformed to dextral strike-slip during 15.5～5.5Ma, and resumed to dextral strike-slip since 5.5Ma.
引文
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冯万鹏,张景发,田云峰.2004.基于ETM+遥感影像红河断裂带构造解释方法.地壳构造与地壳应力文集,(17):161～166.
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向宏发,韩竹军,虢顺民,陈立春,张晚霞.2004.红河断裂带大型右旋走滑运动与伴生构造地貌变形.地震地质,26(4):597～610.
向宏发,万景林,韩竹军,虢顺民,张晚霞,陈立春,董兴权.2006.红河断裂带大型右旋走滑运动发生时代的地质分析与FT测年.中国科学D辑,36(1):977～987.
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张岳桥.2004.晚新生代青藏高原构造挤出及其对中国东部裂陷盆地晚期油气成藏的影响.石油与天然气地质,25(2):162～169.
张志清,刘宇平,陈智梁,唐文清,张选阳,Robert W.King,Barrcel C.Burchfiel.2006.红河断裂的GPS监测.地球学报,27(4):367～372.
朱俊江,詹文欢,唐诚,丘学林.2002.水系的分形特征与红河断裂带活动性关系初探.华南地震,22(1):1～7.
朱俊江,詹文欢,丘学林,徐辉龙,唐诚.2004.红河断裂带两侧地震震源机制及构造意义.大地构造与成矿学,28(3):239～247.
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Lacassin R,Leloup P H,Tapponnier P.1993.Bounds on strain in large shear zones of SE Asia from boudinage restoration.J.Struct.Geol.,15:677～692.
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陈文寄,李齐,汪一鹏.1996.哀牢山-红河走滑剪切带中新世抬升的时间序列.地质论评,42(5):385～390.
邓起东.2002.中国新构造和活动构造研究的新进展.见:陈毓川主编.中国地质学会80周年学术文集.北京:地质出版社,212～221.
冯万鹏,张景发,田云峰.2004.基于ETM+遥感影像红河断裂带构造解释方法.地壳构造与地壳应力文集,(17):161～166.
郝天珧,刘建华,宋海斌,胥颐.2002.华南及其相邻边缘海域一些重要断裂的地球物理证据.地球物理学进展,17(1):13～23.
何廉声,陈邦彦.1987.南海地质地球物理图集.广州:广东地图出版社.
梁狄刚.1999.塔里木盆地九年油气勘探历程与回顾.勘探家:石油与天然气,4(3):57～62.
李齐,陈文寄,万景林,李大明.2000.哀牢山-红河剪切带构造抬升和运动形式转换时间的新证据.中国科学(D辑),30(6):566～583.
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屈春燕,单建新,马瑾.2006.红河断裂红外高温条带的成因及其与地震活动性关系的探讨.地震学报,285(1):91～97.
孙龙涛,孙珍,詹文欢,孙宗勋,赵明辉,夏少红.2006.南海西部断裂系研究及其物理模拟实验证据.海洋学报,28(3):64～71.
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.
孙珍,周蒂,钟志洪,丘学林,曾佐勋.2005.莺-琼盆地基底控制断裂样式的模拟探讨.热带海洋学报,24(2):70～78.
万玲,姚伯初,吴能有.2000.红河断裂入海后的延伸及其构造意义.国土资源部广州海洋地质调查局编,南海地质研究(12).武汉:中国地质大学出版,22～32.
吴进民.1999.南沙万安盆地新生代构造运动和构造演化.海洋地质,2:1～11.
向宏发,韩竹军,虢顺民,陈立春,张晚霞.2004.红河断裂带大型右旋走滑运动与伴生构造地貌变形.地震地质,26(4):597～610.
向宏发,万景林,韩竹军,虢顺民,张晚霞,陈立春,董兴权.2006.红河断裂带大型右旋走滑运动发生时代的地质分析与FT测年.中国科学D辑,36(1):977～987.
姚伯初,邱燕,李唐根.1999.南海西缘-万安断裂的走滑特征及其构造意义.见:姚伯初等主编,南海西部海域地质构造特征和新生代沉积.北京:地质出版社,45～55.
曾维军,李振五,吴能友,陈艺中,杜德莉,温喜文,李国胜.1997.南海区域的上地幔活动特征及印支地幔柱.国土资源部广州海洋地质调查局编,南海地质研究(9),武汉:中国地质大学出版社,1～19.
张培震,邓起东,张国民,马瑾,甘卫军,闵伟,毛凤英,王琦.2003.中国大陆的强震活动与活动地块.中国科学(D辑),33(B04):12～20.
张岳桥.2004.晚新生代青藏高原构造挤出及其对中国东部裂陷盆地晚期油气成藏的影响.石油与天然气地质,25(2):162～169.
张志清,刘宇平,陈智梁,唐文清,张选阳,Robert W.King,Barrcel C.Burchfiel.2006.红河断裂的GPS监测.地球学报,27(4):367～372.
朱俊江,詹文欢,唐诚,丘学林.2002.水系的分形特征与红河断裂带活动性关系初探.华南地震,22(1):1～7.
朱俊江,詹文欢,丘学林,徐辉龙,唐诚.2004.红河断裂带两侧地震震源机制及构造意义.大地构造与成矿学,28(3):239～247.
Allen C R,Gillespie A R,Han Y,Sieh,K E,Zhang Buchun,Zhu Chengnan.1984.Red River and associated faults,Yunnan province,China.Quaternary geology,slip rate and seismic hazard.Bull.Geol.Soc.Am.95,686～700.
Briais A,Patriat P,Tapponnier P.1993.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea,implications for the Tertiary tectonics of SE Asia.J.Geophys.Res.,98:6299～6328.
Gong,Z.,et al.1997.Continental margin basin analysis and hydrocarbon accumulation of the Northern South China Sea.Beijing:Science Press,1～510.
Hall R.1996.Reconstructing Cenozoic SE Asia.In:Hall R,Blundell D J.(eds).Tectonic evolution of southeast Asia.London:Geological Society Special Publication,106:153～184.
He J.1990.Characteristics of mud diapir evolution and oil potential in the Yinggehai Basin.Oil and Gas Geology,11,436～445.
Huang BJ,Xiao X,Zhu W.2004.Geochemistry,origin,and accumulation of CO2in natural gases of the Yinggehai Basin,offshore South China Sea.American Association of Petroleum Geologists Bulletin,88,1277～1293.
Lacassin R,Leloup P H,Tapponnier P.1993.Bounds on strain in large shear zones of SE Asia from boudinage restoration.J.Struct.Geol.,15:677～692.
Le Dain A Y,Tapponnier P,Molnar P.1984.Active faults and tectonics of Burma and surrounding regions.J.Geophys.Res,89:453～472.
Leloup P H.1991.Cine matique des de formations himalayennes''dans la zone de cisaillement crustale de I'Ailao Shan-Fleuve Rouge.These Doctorat,University de Paris VI,148.
Leloup P H,Jean-Robert Kienast.1993.High-temperature metamorphism in a major strike-slip shear zone:the Ailao Shan-Red River,People's Republic of China.Earth and Planetary Science Letters,118:213～234.
Rangin C,Klein M,Roques D,Le Pichon X,Trong LV.1995.The Red River Fault system in the Tonkin Gulf,Vietnam.Tectonophysics,243:209～222.
Leloup P H,Lacassin R,Tapponnier P,Sharer U,Zhong Dalai,Liu Xiaohan,Zhang Liangshang,Ji Shaocheng,Trinh P T.1995.The Ailao Shan Red River shear zone(Yunnan,China),Tertiary transform boundary of Indochina.Tectonophysics(special issue),251(1-4):3～84.
Replumaz A,Lacassin R,Tapponnier P,Leloup P H.2001.Large river offsets and Plio Quaternary dextral slip rate on the Red River Fault(Yunnan,China).J.Geophys.Res.B,[SolidEarth Planets],106(1):819～836.
Roger F,Leloup P H,Marc J,Robin L,Phan T T,Manrice B,Diane S.2000.Long and complex thermal history of the Song Chay metamorphic dome(Northern Vietnam)by multi-system geochronology.Tectonophysics,321:449～466.
Schrer U,Tapponnier P,Lacassin R,Leloup P H,Zhong Dalai,Ji Shaocheng.1990a.Intraplate tectonics in Asia:aprecise age for large scale Miocene movement along the Ailao Shan-Red River fault zone,China.Earth Planet.Sci.Lett.,97:65～77.
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