天然气地球科学 ›› 2010, Vol. 21 ›› Issue (6): 882–889.doi: 10.11764/j.issn.1672-1926.2010.06.882

• 天然气地质学 • 上一篇    下一篇

鄂尔多斯盆地三叠系延长组沉积充填演化及其对印支构造运动的响应

王峰, 田景春, 范立勇, 陈蓉, 邱军利   

  1.  1.成都理工大学“油气藏地质及开发工程”国家重点实验室,四川 成都 610059;
    2.中国石油长庆油田分公司勘探开发研究院,陕西 西安 710021;
    3.中国科学院油气资源研究重点实验室,甘肃 兰州 730000
  • 收稿日期:2010-04-01 修回日期:2010-06-16 出版日期:2010-12-10 发布日期:2010-12-10
  • 通讯作者: 王峰wangfeng07@cdut.cn E-mail:wangfeng07@cdut.cn
  • 作者简介:王峰(1977-),男,陕西汉中人,讲师,博士后,主要从事储层沉积学研究.
  • 基金资助:

    国家重大专项“大型油气田及煤层气开发”项目(编号:2008ZX05007-005)资助.

Evolution of Sedimentary Fillings in Triassic Yanchang Formation  and Its Response to Indosinian Movement in Ordos Basin

WANG Feng, TIAN Jing-Chun, FAN Li-Yong, CHEN Rong, QIU Jun-Li   

  1. 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,
    Chengdu 610059,China; 2.Research Institute of Exploration and Development,Changqing Oilfield Company
    of CNPC,Xi′an 710021,China; 3.Key Laboratory of Petroleum Resources Research,Instituteof Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000,China  
  • Received:2010-04-01 Revised:2010-06-16 Online:2010-12-10 Published:2010-12-10

摘要:

通过对鄂尔多斯盆地三叠系延长组地层发育特征、湖盆充填演化、盆地边缘沉积特征以及事件沉积发育规律的分析,探讨了早印支运动与鄂尔多斯盆地的沉积响应过程。研究表明,长10—长9沉积期,印支运动较弱,鄂尔多斯盆地基本继承了晚海西期以来的构造平稳的格局,湖盆开始发育;从长8沉积末期开始,鄂尔多斯盆地南部构造活动开始增强,秦岭造山带在该时期迅速隆升使北秦岭地区沿商丹断裂带发育一系列山间盆地的砾岩堆积,同时导致盆地南部海相碳酸盐岩基底遭受剥蚀,碳酸盐岩岩屑在砂岩中开始出现;长7沉积期,伴随着湖盆的强烈扩张、西南部磨拉石建造的快速堆积以及事件沉积频发,印支运动活动强烈,鄂尔多斯盆地进入板块碰撞拼接、幕式构造运动最活跃的时期;长6—长4+5沉积期,鄂尔多斯盆地西南部地层中仍有震积岩出现,但凝灰岩含量急剧减少,表明构造活动的强度和频率降低,湖盆开始重新进入稳定沉降期。延长期湖盆演化随着印支运动发展经历了初始拗陷、强烈拗陷、回返抬升和萎缩消亡的完整过程,具有快速沉降、缓慢充填、沉积中心不断向西南迁移的特征。

关键词: 沉积响应, 构造演化, 延长组, 鄂尔多斯盆地

Abstract:

Based on stratigraphy,lake basin fillings,basin margin sediments,and regularity of event deposits in the Triassic Yanchang Formation,we discussed the early Indosinian event and sedimentary response in Ordos basin.The results indicated that the Indosinian movement was weak within 9 and 10 intervals of Yanchang Formation,the basin inherited the structurally smooth pattern since late Hercynian,and the lake basin began to develop.At 8 interval of Yanchang Formation,the Qinling orogenic uplift made the basin tectonic activity increase rapidly,associated with a series of mountain basin conglomerate in the north Qinling area along Shangdan fault and denudation of marine carbonate strata in the southern basin.The carbonate debris was mixed into the sandstone.At 7 interval of Yanchang Formation,the molasse was deposited rapidly in the southwest with the strong expansion of the lake basin,associated with frequent deposit events.At Indosinian era,the Ordos basin was in the most active period of plate collision splicing and episodic tectonic movements.At time from interval 6 to interval 4,seismites existence and large decrease of tuff content in the strata of southwest basin suggested that the intensity and frequency of tectonic activity would decrease,and the lake basin re-enter the stable subsidence period.With development of the Indosinian movement,the lake basin underwent a complete structural process,including initial depression,a strong depression,up and down,and atrophy,associated with rapid subsidence,slow filling and deposition center continued to migrate southwestward.

Key words: Sedimentary response, Structural evolution, Yanchang Formation, Ordos basin.

中图分类号: 

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[1]Yang Junjie.Tectonic Evolution and Oil-Gas Reservoirs Distribution in Ordos Basin[M].Beijing:Petroleum Industry Press,2002:130-181.[杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002:130-181.]
[2]Yang Youyun.Influence of Qinling orogenic movements in Indo-Chinese epoch to sedimentary characteristics of Yanchang Formation in Ordos basin[J].Coal Geology & Exploration,2004,32(5):7-9.[杨友运.印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响[J].煤田地质与勘探,2004,32(5):7-9.]
[3]Yang Shengbin,Guo Qingyin,Hou Guiting,et al.Subsidence history and sedimentary response in the north of western Ordos basin[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2006,42(2):192-198.[杨圣彬,郭庆银,侯贵廷,等.鄂尔多斯盆地西缘北段沉降史与沉积响应[J].北京大学学报:自然科学版,2006,42(2):192-198.
[4]Deng Xiuqin,Lin Fangxiao,Liu Xianyang,et al.Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the early Indosinian movement in Ordos basin[J].Journal of Palaeogeography,2008,10(2):159-165.[邓秀芹,蔺昉晓,刘显阳,等.鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的讨论[J].古地理学报,2008,10(2):159-165.]
[5]Wang Feng.Study on Sedimentary,Sequence Evolution and Lithologic Oil Pool of Yanchang Formation in Triassic,Ordos Basin[D].Chengdu:Chengdu University of Technology,2007:14-20.[王峰.鄂尔多斯盆地三叠系延长组沉积、层序演化及岩性油藏特征研究[D].成都:成都理工大学,2007:14-20.]
[6]Wu Zhiping,Hou Xubo,Li Wei.Discussion on Mesozoic basin patterns and evolution in the eastern north China block[J].Geotectonica et Metallogenia,2007,31(4):385-399.[吴智平,侯旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399.]
[7]Xia Bangdong,Li Peijun.Sedimentologic evidence on the docking of Yangtse plate and north China plate in middle-late Triassic Period in east China[J].Acta Sedimentologica Sinica,1996,14(1):12-20.[夏邦栋,李培军.中国东部扬子板块同华北板块在中晚三叠世拼接的沉积学证据[J].沉积学报,1996,14(1):12-20.]
[8]Wu Zhiyu,Zhao Hong,Li Wenhou,et al.Sequence stratigraphy of Yanchang Formation in Ansai district[J].Natural Gas Geoscience,2005,16(2):190-193.[吴志宇,赵虹,李文厚,等.安塞地区延长组层序地层特征[J].天然气地球科学,2005,16(2):190-193.]
[9]Wang Hongbo,Zheng Ximin,Feng Ming.Sequence stratigraphy and sources-reservoir-cap assemblages of Yanchang Formation in Ordos basin[J].Natural Gas Geoscience,2006,17(5):677-681.[王宏波,郑希民,冯明.鄂尔多斯盆地三叠系延长组层序地层与生储盖组合特征[J].天然气地球科学,2006,17(5):677-681.]
[10]Li Wenhou,Pang Jungang,Cao Hongxia ,et al.Depositional system and paleogeographic evolution of the late Triassic Yanchang Stage in Ordos basin[J].Journal of Northwest University:Natural Science Edition,2009,39(3):501-506.[李文厚,庞军刚,曹红霞,等.鄂尔多斯盆地晚三叠世延长组沉积体系及岩相古地理演化[J].西北大学学报:自然科学版,2009,39(3):501-506.]
[11]Zhao Wenzhi,Hu Suyun,Wang Zecheng,et al.Key role of basement fault control on oil accumulation of Yanchang Formation,upper Triassic,Ordos basin[J].Petroleum Exploration and Development,2003,30(5):1-6.[赵文智,胡素云,汪泽成,等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用[J].石油勘探与开发,2003,30(5):1-6.]
[12]Wang Feng,Liu Chiyang,Yang Xingke,et al.Geologic geochemical features of basalt in Ruqi clough of Helan mountain and its structural environmental significance[J].Petroleum Geology & Oilfield Development in Daqing,2005,24(4):25-27.[王锋,刘池阳,杨兴科,等.贺兰山汝箕沟玄武岩地质地球化学特征及其构造环境意义[J].大庆石油地质与开发,2005,24(4):25-27.]
[13]Bai Yunlai,Wang Xinmin,Liu Huaqing,et al.Determination of the borderline of the western Ordos basin and its geodynamics background[J].Acta Geologica Sinica,2006,80(6):793-810.[白云来,王新民,刘化清,等.鄂尔多斯盆地西部边界的确定及其地球动力学背景[J].地质学报,2006,80(6):793-810.]
[14]Liu Huaqing,Li Xiangbo,Bai Yunlai,et al.Origin analysis of the “Kongtong Conglomerate” in Ordos basin[J].Natural Gas Geoscience,2006,17(5):668-671.[刘化清,李相博,白云来,等.鄂尔多斯盆地“崆峒山砾岩”成因初步分析[J].天然气地球科学,2006,17(5):668-671.]
[15]Yang Zhenyu,Ma Xinghua,Huang Baochun,et al.North China block Phanerozoic paleomagnetic Apparent polar wander paths and block movement[J].Science in China:D Series,1998,28(supplement):44-56.[杨振宇,马醒华,黄宝春,等.华北地块显生宙古地磁视极移曲线与地块运动[J].中国科学:D辑,1998,28(增刊):44-56.]
[16]Zhao Junxing,Chen Hongde,Fu Suotang,et al.Discussion on some important depositional events and their relationship with hydrocarbon accumulation of Yanchang Formation in south Ordos basin[J].Journal of Mineralogy and Petrology,2008,28(3):91-95.[赵俊兴,陈洪德,付锁堂,等.鄂尔多斯盆地南部延长组中几个重要事件沉积及其油气聚集关系[J].矿物岩石,2008,28(3):91-95.]
[17]Xia Qingsong,Tian Jingchun.Characteristics and geological significance of seismites of the Yanchang Formation,upper Triassic,Ordos basin[J].Acta Geologica Sinica,2007,25(2):246-252.[夏青松,田景春.鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义[J].沉积学报,2007,25(2):246-252.]
[18]Shao Xiaoyan,Tian Jingchun,Zhang Jinquan,et al.Paleo-seismic records of Chang 4+5 oil-bearing intervals of the upper Triassic Yanchang Formation in Ordos basin[J].Journal of Palaeogeography,2009,11(2):177-185.[邵晓岩,田景春,张锦泉,等.鄂尔多斯盆地上三叠统延长组长4+5油层组中的古地震记录[J].古地理学报,2009,11(2):177-185.]
[19]Yang Youyun,Zhang Pengbo,Zhang Zhongyi.Sedimentary features and sequence evolution of braided river delta of Chang 8 oil Formation of Xifeng oilfield in Ordos basin[J].Geological Science and Technology Information,2005,24(1):45-48.[杨友运,张蓬勃,张忠义.鄂尔多斯盆地西峰油田长8油组辫状河三角洲沉积特征与层序演化[J].地质科技情报,2005,24(1):45-48.]
[20]Chen Gang.Terrigenous clastic composition and its tectonic feature in the Mesozoic of the Ordos basin[J].Acta Sedimentologica Sinica,1999,17(3):409-413.[陈刚.中生代鄂尔多斯盆地陆源碎屑成分及其构造属性[J].沉积学报,1999,17(3):409-413.]
[21]Lu Kezheng,Qi Jiafu,Dai Junsheng.The Structural Model of Cenozoic Hydrocarbon Basin in Bohai Bay [M].Beijing:Geological Press,1997:1-3.[陆克政,漆家福,戴俊生.渤海湾新生代含油气盆地构造模式[M].北京:地质出版社,1997:1-3.]
[22]Fang Dajun,Wu Nengyou,Jin Guohai.Preliminary study of paleomagnetism and tectonic evolution of western Zhejiang and Anhui Paleozoic in Yangtze plate[J].Chinese Science Bulletin,1992,35(6):543-546.[方大钧,吴能友,金国海.扬子板块浙西、皖南古生代岩石古地磁结果与构造演化的初步探讨[J].科学通报,1992,35(6):543-546.]
[23]Liu Shaofeng,Yang Shigong.The difference between the northwestern and southwestern Ordos basin and their formation mechanism[J].Scientia Geologica Sinica,1997,32(3):397-408.[刘少峰,杨士恭.鄂尔多斯盆地西缘南北差异及其形成机制[J].地质科学,1997,32(3):397-408.]
[24]Yu Hezhong,Lv Fuliang,Guo Qingxin,et al.Proto-sediment basin types and tectonic evolution in the southern edge of north China plate[J].Petroleum Geology and Expeximent,2005,27(2):111-117.[余和中,吕福亮,郭庆新,等.华北板块南缘原型沉积盆地类型与构造演化[J].石油实验地质,2005,27(2):111-117.]
 [25]Zhang Guowei,Meng Qingren,Yu Zaiping,et al.The orogenic process and dynamic characteristics of Qinling orogenic belt[J].Science in China:Series D,Earth Science,1996,26(3):193-200.[张国伟,孟庆任,于在平,等.秦岭造山带的造山过程及其动力学特征[J].中国科学:D辑,地球科学,1996,26(3):193-200.]
[26]Wang Hongzhen.Atlas of the Palaeogeography of China[M].Beijing:Carto-graphic PublishingHouse,1985.[王鸿桢.中国古地理图集[M].北京:地图出版社,1985.]
[27]Zhai Guangming,Song Jianguo,Jin Jiuqiang,et al.Plate Tectonic Evolution and Its Relationship to Petroliferous Basins[M].Beijing:Petroleum Industry Press,2002:2-63.[翟光明,宋建国,靳久强,等.板块构造演化与含油气盆地形成和评价[M].北京:石油工业出版社,2002:2-63]

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