齐古断褶带构造演化研究
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摘要
针对准噶尔盆地南缘齐古断褶带复杂构造情况,开展了齐古断褶带构造演化研究。在广泛调研天山山体演化、周边地层发育、地表水流变更、地震解释剖面的基础上,以理论地质学为指导,结合研究区内头屯河三叠系—新近系的标准地层剖面、地面地质详查资料、重要地震勘探解释剖面、综合研究报告等资料,研究了喜马拉雅期齐古断褶带平面构造特征、齐古断褶带剖面构造特征,分析了齐古断褶带的主要构造特征,划分出了齐古断褶带的构造模式。研究认为:齐古断褶带构造演化可划分为四个阶段,依次为掀斜阶段、断褶阶段、滑脱阶段和楔入阶段。为齐古断褶带下步油气勘探提供了依据。
Aiming at complex structure of Qigu fault-folded belts in Junggar Basin,structural evolution is studied in this paper.ByinvestigatingmassifevolutionofMountTianshan,stratumdevelopmentofsurrounding,thechangeofsurfacewater,seismic interpret profile,regarding theoretical geology as guidelines,combining standard stratigraphic section of between Triassic and Neozoic,surface geology data,important interpretation profile of seismic exploration,integrated research report,plane and profile structural characteristics of Qigu fault-folded belts in the period of Himalaya are researched in this paper.The main structural characteristics of Qigu fault-folded belts is analysed and its structural model is divided.In this paper,it is considered that the structural evolution of Qigu fault-folded belts is divided into four stages,including tilt stage,fault-folded stage,detachment stage and wedging stage.It provides proof to exploration of Qigu fault-folded belts.
Aiming at complex structure of Qigu fault-folded belts in Junggar Basin,structural evolution is studied in this paper.ByinvestigatingmassifevolutionofMountTianshan,stratumdevelopmentofsurrounding,thechangeofsurfacewater,seismic interpret profile,regarding theoretical geology as guidelines,combining standard stratigraphic section of between Triassic and Neozoic,surface geology data,important interpretation profile of seismic exploration,integrated research report,plane and profile structural characteristics of Qigu fault-folded belts in the period of Himalaya are researched in this paper.The main structural characteristics of Qigu fault-folded belts is analysed and its structural model is divided.In this paper,it is considered that the structural evolution of Qigu fault-folded belts is divided into four stages,including tilt stage,fault-folded stage,detachment stage and wedging stage.It provides proof to exploration of Qigu fault-folded belts.
引文
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[16]王兆明,罗晓容,刘楼军,等.准噶尔盆地南缘霍–玛–吐断层活动特征及成藏过程[J].石油学报,2006,27(5):28–34.Wang Zhaoming,Luo Xiaorong,Liu Loujun,et al.Ac-tive features of Huo2Ma2Tu fault and hydrocarbon accu-mulation in the southern Junggar Basin[J].Acta Petrolei Sinica,2006,27(5):28–34.
[17]旷理雄,郭建华,童小兰,等.准噶尔盆地南缘东段油气成藏条件及成藏模式[J].地球科学与环境学报,2007,29(1):34–41.Kuang Lixiong,Guo Jianhua,Tong Xiaolan,et al.Form-ing Conditions and Patterns of Hydrocarbon Reservoirs in East of Southern Fringe of Junggar Basin[J].Journal of Earth Sciences and Environment,2007,29(1):34–41.
[18]宋永东,戴俊生,吴孔友.准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式[J].西安石油大学学报:自然科学版,2009,24(3):17–20.Song Yongdong,Dai Junsheng,Wu Kongyou.Study on the structural features and hydrocarbon accumulation-modes of Wuxia fault be lt in the northw estmargin of JunggarBasin[J].JournalofXi’anShiyouUniversity:Sci-ence&Technology Edition,2009,24(3):17–20.
[19]邵雨,陈伟,张伯友.断层相关褶皱理论在准噶尔盆地南缘山前带构造研究的应用[J].地球科学与环境学报,2005,27(1):26–30.Shao Yu,Chen Wei,Zhang Boyou.Application of the geometry of faul-t related folding to the southern Jung-gar Basin[J].Journal of Earth Sciences and Environment,2005,27(1):26–30.
[2]邓启东,冯先岳,张培震,等.天山活动构造[M].北京:地震出版社,2000.
[3]李德江,杨俊生,朱筱敏.准噶尔盆地层序地层学研究[J].西安石油大学学报:自然科学版,2005,20(3):60–66.Li Dejiang,Yang Junsheng,Zhu Xiaomin.Study on thesequence stratigraphy of Junggar Basin[J].Journal ofXi’an Shiyou University:Science&Technology Edition,2005,20(3):60–66.
[4]况军,贾希玉.喜马拉雅运动与准噶尔盆地南缘油气成藏[J].新疆石油地质,2005,26(2):129–133.Kuang Jun,Jia Xiyu.Relationship between HimalayanMovement and Hydrocarbon Aecumulation in SouthernMargin of Junggar Basin[J].Xinjiang Petroleum Geolo-gy,2005,26(2):129–133.
[5]况军,朱新亭.准噶尔盆地南缘托斯台地区构造特征及形成机制[J].新疆石油地质,1990,11(2):95–101.Kuang Jun,Zhu Xinting.Characteristics and Mechanismof Formation of Structures in Tousitai Area,South Mar-gin,Juggar Basin[J].Xinjiang Petroleum Geology,1990,11(2):95–101.
[6]况军.准噶尔盆地南缘西段的重力构造[J].石油与天然气地质,1990,11(3):275–282.Kuang Jun.Gravity Structures in West Part of SouthMargin of Junggar Basin[J].Oil&Gas Geology,1990,11(3):275–282.
[7]吕红华,李有利,南峰,等.天山北麓河流阶地序列及形成年代[J].地理学报,2008,63(1):65–74.Lv Honghua,Li Youli,Nan Feng et al.Sequences andAges of Fluvial Terraces along the Northern Piedmon-t of the Tianshan Mountains[J].Acta Geographica Sinica,2008,63(1):65–74.
[8]王永,王彦斌.北天山山前安集海河阶地形成的时代及意义[J].地质论评,2000,46(6):584–587.Wang Yong,Wang Yanbin.Formation of the Anjihai Riv-er Terraces at the North Tianshan Piedmont,Xinjiang,and Significance[J].Geological Review,2000,46(6):584–587.
[9]史兴民,杨景春,李有利,等.天山北麓玛纳斯河河流阶地变形与新构造运动[J].北京大学学报:自然科学版,2004,40(6):971–978.Shi Xingmin,Yang Jingchun,LI Youli,et al.De-formation of Manas River Terraces and Neotectonicsin Northern Front of the Tianshan Mountains[J].ActaScientiarum Naturalium Universitatis Pekinensis,2004,40(6):971–978.
[10]刘全稳.理论地质学导论[M].北京:地质出版社,2006.
[11]刘全稳,赵金洲,陈景山.地球动力与运动[M].北京:地质出版社,2001.
[12]张培震,邓起东,徐锡伟,等.天山北麓玛钠斯活动逆断裂-褶皱带的变形特征与构造演化.活动断裂研究(3)[M].北京:地震出版社,1994,18–32.
[13]胡玲,何登发,胡道功.准噶尔盆地南缘霍尔果斯–玛纳斯–吐谷鲁断裂晚新生代构造变形的ESR测年证据[J].地球学报,2005,26(2):121–126.Hu Ling,He Dengfa,Hu Daogong.Electron Spin Res-onance Dating of the Late Cenozoic Deformation of theHuoerguosi-Manas-Tugulu Reverse Faults along South-ern Edge of Junggar Basin[J].Acta Geoscientica Sinica,2005,26(2):121–126.
[14]武富礼,姚志刚.碎屑锆石U–Pb定年在准噶尔盆地南缘物源研究中的应用[J].西安石油大学学报:自然科学版,2011,26(3):6–13.Wu Fuli,Yao Zhigang.Application of U–Pb dating inthe study on the provenance analysis of detrital zircons inthe southern margin of Junggar Basin[J].Journal of Xi’anShiyou University:Science&Technology Edition,2011,26(3):6–13.
[15]李忠权,张寿庭,应丹琳,等.准噶尔盆地南缘托斯台地区构造特征研究[J].成都理工大学学报:自然科学版,2010,37(6):593–598.Li Zhongquan,Zhang Shouting,Ying Danlin,et al.ThecharacteristicsofthestructuresectioninTuositairegiononthesouthedgeofJunggarBasin[J].Journal of Chengdu U-niversity of Technology:Science&Technology Edition,2010,37(6):593–598.
[16]王兆明,罗晓容,刘楼军,等.准噶尔盆地南缘霍–玛–吐断层活动特征及成藏过程[J].石油学报,2006,27(5):28–34.Wang Zhaoming,Luo Xiaorong,Liu Loujun,et al.Ac-tive features of Huo2Ma2Tu fault and hydrocarbon accu-mulation in the southern Junggar Basin[J].Acta Petrolei Sinica,2006,27(5):28–34.
[17]旷理雄,郭建华,童小兰,等.准噶尔盆地南缘东段油气成藏条件及成藏模式[J].地球科学与环境学报,2007,29(1):34–41.Kuang Lixiong,Guo Jianhua,Tong Xiaolan,et al.Form-ing Conditions and Patterns of Hydrocarbon Reservoirs in East of Southern Fringe of Junggar Basin[J].Journal of Earth Sciences and Environment,2007,29(1):34–41.
[18]宋永东,戴俊生,吴孔友.准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式[J].西安石油大学学报:自然科学版,2009,24(3):17–20.Song Yongdong,Dai Junsheng,Wu Kongyou.Study on the structural features and hydrocarbon accumulation-modes of Wuxia fault be lt in the northw estmargin of JunggarBasin[J].JournalofXi’anShiyouUniversity:Sci-ence&Technology Edition,2009,24(3):17–20.
[19]邵雨,陈伟,张伯友.断层相关褶皱理论在准噶尔盆地南缘山前带构造研究的应用[J].地球科学与环境学报,2005,27(1):26–30.Shao Yu,Chen Wei,Zhang Boyou.Application of the geometry of faul-t related folding to the southern Jung-gar Basin[J].Journal of Earth Sciences and Environment,2005,27(1):26–30.
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