黔南坳陷及邻区盆地演化和海相沉积的后期改造

doi:10.7605/gdlxb.2012.04.009

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Abstract The southern Guizhou Depression，bounded by the Guiyang-Zhenyuan，Ziyun-Luodian and Tongren-Sandu faults on the north，southwest and east respectively，is a relatively stable block within the Yangtze Craton.The tectono-palaeogeographic evolution of the depression and its neighboring areas could be divided into four stages: Neoproterozoic，Early Paleozoic，Late Paleozoic-Triassic，Jurassic-Paleogene，and the basin development coupling with the neighboring orogenesis was reconstructed.The Guangxi orogeny was an important reformation in the formation period of marine sediments，which resulted in appearance of NE-striking structures.The Indosinian orogeny caused the NEE-orientation Guiyang-Zhenyuan fault and the NW-orientation Ziyun-Luodian fault inverted，and founded the north and southwest boundaries of the southern Guizhou Depression for the both faults.The NE-striking faults rejuvenated repeatedly in Meso-Cenozoic.Two generations of thrusting since the Middle Jurassic could be distinguished.The early one occurred in the Yanshanian orogeny，with the thrusting towards the northwest，and the thrust system expanding to the northwest.The later one occurred in the latest Yanshanian-Himalayan orogeny.Regionally，the NNE-striking faults thrust towards the east to south，and the Tongren-Sandu fault became east boundary of the southern Guizhou Depression.The longitudinal faults within the depression，which created in the Indosinian orogeny，rejuvenated and thrust towards the west，and made up a back-thrust system of the Tongren-Sandu fault in the latest Yanshanian-Himalayan orogeny.The broad folds developed in the upper plates of the longitudinal faults might be beneficial target regions for marine oil-gas exploration in the depression.

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	Articles by authors
	Wu Genyao
	Wang Weifeng
	Chi Hongxing

Key words： southern Guizhou Depression tectono-palaeogeographic evolution basin-orogeny coupling Guangxi orogeny Indosinian orogeny Yanshanian orogeny latest Yanshanian-Himalayan orogeny oil-gas exploration

Received: 19 August 2011 Published: 01 August 2012

ZTFLH:

P548

About author: Wu Genyao，born in 1946，graduated from the Department of Geology，Peking University in 1968 and obtained his Ph.D.degree in 1985.Now he majors in tectonics.

Cite this article:

Wu Genyao,Wang Weifeng,Chi Hongxing. Basin evolution and later reformation of marine sediments in southern Guizhou Depression and neighboring areas[J]. JOURNAL OF PALAEOGEOGRAPHY, 2012, 14(4): 507-521.

Wu Genyao,Wang Weifeng,Chi Hongxing. Basin evolution and later reformation of marine sediments in southern Guizhou Depression and neighboring areas[J]. JOPC, 2012, 14(4): 507-521.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2012.04.009 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2012/V14/I4/507

陈海泓，孙枢，李继亮，等.1992.前陆盆地的构造制约——以湘西中生代沅麻盆地为例［M］.见:李继亮.中国东南海陆岩石圈结构与演化研究.北京:中国科学技术出版社，17-31.
戴传固，陈建书，卢定彪，等.2010.黔东南及邻区加里东运动的表现及地质意义［J］.地质通报，29（4）:530-534.
冯增昭，鲍志东，李尚武.1997.中国南方早中三叠世岩相古地理［M］.北京:石油工业出版社，1-179.
甘晓春，李献华，赵风清，等.1996.广西龙胜丹州群细碧角斑岩锆石U-Pb及Sm-Nd等时线年龄［J］.地球化学，25（3）:270-276.
贵州省地质矿产局.1987.贵州省区域地质志［M］.北京:地质出版社，1-698.
何治亮，汪新伟，李双建，等.2011.中上扬子地区燕山运动及其对油气保存的影响［J］.石油实验地质，33（1）:1-11.
邝国敦，吴浩若.2002.桂西晚古生代深水相地层［J］.地质科学，37（2）:152-164.
匡文龙，杨绍祥，余沛然，等.2008.湘西北花垣县下寒武统清虚洞组浊积岩沉积特征及其地质意义［J］.地质科学，43（2）:347-358.
梁继涛，张德宝，薄志宏.1991.“华夏古陆”考异［J］.中国地质科学院南京地质矿产研究所所刊，12（3）:3-12.
梁新权，郭定良.2002.湖南深部构造活化及其浅部响应［J］.地质科学，37（3）:332-342.
刘鸿允，等.1991.中国震旦系［M］.北京:科学出版社，1-388.
马力，陈焕疆，甘克文，等.2004.中国南方大地构造和海相油气地质［M］.北京:地质出版社，71-84，104-146，180-255，513-543.
马文璞，李学军，刘和甫，等.1993.雪峰隆起的构造性质及其对上扬子东南缘古生代盆地的改造［M］.见:张渝昌等编.江南—雪峰地区的层滑作用及多期复合构造.北京:地质出版社，120-147.
丘元禧，陈焕疆（主编）.1993.云开大山及其邻区地质构造论文集［M］.北京:地质出版社，1-11，35-43.
时国，田景春，喻美艺.2008.贵阳花溪地区早—中三叠世碳酸盐岩角砾岩楔沉积特征［J］.古地理学报，10（5）:521-528.
汤良杰，郭彤楼，田海芹，等.2008.黔中地区多期构造演化、差异变形与油气保存条件［J］.地质学报，82（3）:298-307.
万方，许效松.2003.川滇黔桂地区志留纪构造—岩相古地理［J］.古地理学报，5（2）:180-186.
王剑.2005.华南“南华系”研究新进展——论南华系地层的划分与对比［J］.地质通报，24（6）:491-495.
吴根耀.1998a.华南及邻区特提斯演化［M］.见：曹佑功.全球构造带、超大陆形成与裂解.北京：地质出版社，46-63.
吴根耀.1998b.盆地研究的活动论构造观［J］.石油实验地质，20（4）:309-318.
吴根耀.2000a.华南的格林威尔造山带及其坍塌: 在罗迪尼亚超大陆演化中的意义［J］.大地构造与成矿学，24（2）:112-123.
吴根耀.2000b.造山带地层学［M］.四川成都:四川科学技术出版社；新疆乌鲁木齐:新疆科技卫生出版社，1-218.
吴根耀.2001.滇桂交界区印支期前陆褶皱冲断带［J］.地质科学，36（1）:64-71.
吴根耀.2002.燕山运动和中国大陆晚中生代的活化［J］.地质科学，37（4）:453-461.
吴根耀.2005.造山带古地理学——在盆地构造古地理重建中的若干思考［J］.古地理学报，7（3）:405-416.
吴根耀.2007.造山带古地理学——重建区域构造古地理的若干思考［J］.古地理学报，9（6）:635-650.
吴根耀，李曰俊.2011.桂东南马山沿灵山断裂出露的印支期洋岛玄武岩及其区域构造意义［J］.现代地质，25（4）:682-691.
吴根耀，马力.2002.“盆”“山”耦合与脱耦: 含油气盆地研究的新思路［M］.见:中国石油学会石油地质专业委员会编.油气盆地研究新进展第一辑.北京:石油工业出版社，21-36.
吴根耀，符鹤琴，汤家富.1998.赣东北地区晚元古代登山群火山岩的特点及其形成的大地构造背景［J］.岩石学报，14（2）:240-250.
吴根耀，梁兴，陈焕疆.2007.试论郯城—庐江断裂带的形成、演化及其性质［J］.地质科学，42（1）:160-175.
吴根耀，梁兴，马力.2009.扬子克拉通继承性构造与新生构造并存的时空发育特征及其对海相油气勘探的指导［J］.石油实验地质，31（1）:1-11，18.
吴根耀，马力，许效松，等.2001b.喜马拉雅运动：对川滇交界区古地理重建的制约和楚雄盆地的改造［J］.古地理学报，3（2）:3-10.
吴根耀，马力，钟大赉，等.2001a.滇桂交界区印支期增生弧型造山带: 兼论与造山作用耦合的盆地演化［J］.石油实验地质，23（1）:8-18.
吴根耀，王晓鹏，钟大赉.1999.藏东南地区早白垩世的安第斯型弧火山岩［J］.岩石学报，15（3）:422-429.
许效松，尹福光，万方，等.2001.广西钦州海槽迁移与沉积—构造转换面［J］.沉积与特提斯地质，21（4）:1-10.
许效松，刘伟，周棣康，等.2009.黔中—黔东南下志留统沉积相［J］.古地理学报，11（1）:13-20.
徐政语，姚根顺，郭庆新，等.2010.黔南坳陷构造变形特征及其成因解析［J］.大地构造与成矿学，34（1）:20-31.
张启锐，储雪蕾.2007.南华系建系问题探讨［J］.地层学杂志，31（3）:222-228.
张秀庭.1992.施洞口地区的逆冲推覆作用及其基本特征［J］.贵州地质，8（2）:135-142.
钟大赉，等.1998.滇川西部古特提斯造山带［M］.北京：科学出版社，1-231.
Chung S-L，Jahn B M.1995.Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary［J］.Geology，（10）:889-892.
Chung S-L，Jahn B M，Wu G Y， et al.1998.The Emeishan Flood Basalt in SW China: A Mantle Plume Initiation Model and Its Connection with Continental Breakup and Mass Extinction at the Permian-Triassic Boundary［M］.In: Flower M F J，Chung S-L，Lo C-H，et al.（eds）.Mantle Dynamics and Plate Interaction in East Asia.U.S.A. Washington D C: American Geophysical Union，47-58.
Wu G Y.1998.Early Paleozoic accretion and amalgamation in a Gondwana-originated China［J］.Acta Universitatis Calolinae——Geologica，42（3-4）:501-507.
Wu G Y.2000.Rejuvenation of fossil sutures and related Mesozoic intracontinental orogens in South China［J］.Acta Geologica Sinica（English Ed.），74（2）:194-200.
Wu G Y，Tang J F.1997.Wugong Mts.Region as a Caledonian medium-high pressure metamorphic belt: Evidence from b₀ values of white micas［J］.Geotectonica et Metallogenia，21（1-2）: 51-55.
Wu G Y，Yano T，Inomata M.1998.Yanshanian orogenics in South China: A relation to Neotethyan evolution［J］.Scientia Geologica Sinica，7（1）:1-10.
Wu G Y，Zhong D L，Zhang Q， et al.1999.Babu—Phu Ngu ophiolites: A geological record of Paleotethyan ocean bordering China and Vietnam［J］.Gondwana Research，2（4）:554-557.