Advanced Search
Volume 40 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(3): 303-314
XU Xi, ZHU Xiaoying, SHAN Xipeng, XIAO Mengchu, SUN Lianpu, GAO Shunli. Structure and sedimentary characteristics of the Meso-Cenozoic basin group along the Yangtze River in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(3): 303-314. doi: 10.11781/sysydz201803303
Citation: XU Xi, ZHU Xiaoying, SHAN Xipeng, XIAO Mengchu, SUN Lianpu, GAO Shunli. Structure and sedimentary characteristics of the Meso-Cenozoic basin group along the Yangtze River in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(3): 303-314. doi: 10.11781/sysydz201803303
shu

Structure and sedimentary characteristics of the Meso-Cenozoic basin group along the Yangtze River in the Lower Yangtze region

doi: 10.11781/sysydz201803303
  • 1.

    China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China

  • 2. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China

  • 3. Sino Getech(Beijing) Science & Technology Co., Ltd., Beijing 100015, China

  • 4. Shanghai Branch of CNOOC China Ltd., Shanghai 200030, China

  • Received Date: 2017-07-04
  • Rev Recd Date: 2018-03-28
  • Publish Date: 2018-05-28
    Abstract
  • The basin group along the Yangtze River is an important part of the Meso-Cenozoic petroliferous basins in the Lower Yangtze region, which is also an important window for the study of the structure and tectono-sedimentary evolution of the Meso-Cenozoic basins in East China. There are nine relatively independent faulted basins from west to east in the Yangtze River's middle and lower reaches, including Poyang, Qianshan, Wanjiang, Quanjiao, Wuwei, Jurong-Nanling, Changzhou-Xuancheng, Liyang and Pinghu basins, which comprise a basin system or group in the plane, named the Lower Yangtze basin group. Sedimentary filling in the basins was divided into two stages including faulting from the Late Cretaceous to the Paleogene, and depression from the Neogene to the Quaternary. The former stage is characterized by the sedimentation of fluviolacustrine and delta facies, while the latter stage is marked by the deposition of fluvial facies. The fault basin system formed in the Late Oligocene, and a unified depression system formed in the Neogene along the Yangtze River. Due to the Neogene differential deformation, the basinal strata were differentially denuded, forming the modern geological setting of the sedimentary basins.

     

    • FullText(HTML)
  • loading
    • References(40)
  • [1]
    徐曦,高顺莉.下扬子区新生代断陷盆地的构造与形成[J].地学前缘,2015,22(6):148-166. XU Xi,GAO Shunli.The structure and formation of the Cenozoic fault basin in the Lower Yangtze region[J].Earth Science Frontiers,2015,22(6):148-166.
    [2]
    徐曦,高顺莉,王兴建,等.下扬子区新生代伸展构造变形及其区域构造意义[J].地球科学(中国地质大学学报),2015,40(12):1968-1986. XU Xi,GAO Shunli,WANG Xingjian,et al.Cenozoic deformation of extensional tectonics in the Lower Yangtze region and its tectonic significance[J].Earth Science(Journal of China University of Geoscience),2015,40(12):1968-1986.
    [3]
    马立桥,陈汉林,董庸,等.苏北-南黄海南部叠合盆地构造演化与海相油气勘探潜力[J].石油与天然气地质,2007,28(1):35-42. MA Liqiao,CHEN Hanlin,DONG Yong,et al.Tectonic evolution of Subei-South Nanhuanghai superimposed basin from the Late Mesozoic to the Cenozoic and marine petroleum potential[J].Oil & Gas Geology,2007,28(1):35-42.
    [4]
    江夏,周荔青.苏北盆地富油气凹陷形成与分布特征[J].石油实验地质,2010,32(4):319-325. JIANG Xia,ZHOU Liqing.Characteristics of formation and distribution of prolific sags in the Northern Jiangsu Basin[J].Petroleum Geology & Experiment,2007,32(4):319-325.
    [5]
    朱光,姜芹芹,朴学峰,等.基底断层在断陷盆地断层系统发育中的作用:以苏北盆地南部高邮凹陷为例[J].地质学报,2013,87(4):441-452. ZHU Guang,JIANG Qinqin,PIAO Xuefeng,et al.Role of basement faults in faulting system development of a rift basin:An example from the Gaoyou Sag in southern Subei Basin[J].Acta Geologica Sinica,2013,87(4):441-452.
    [6]
    胡红雷,朱光.苏北地区前陆变形特征与形成机制[J].大地构造与成矿学,2013,37(3):366-376. HU Honglei,ZHU Guang.Characteristics and formation mechanism of the foreland deformation in the Subei region[J].Geotectonica et Metallogenia,2013,37(3):366-376.
    [7]
    朱光,徐嘉炜,刘国生,等.下扬子地区前陆变形构造格局及其动力学机制[J].中国区域地质,1999,18(1):73-79. ZHU Guang,XU Jiawei,LIU Guosheng,et al.Tectonic pattern and dynamic mechanism of the foreland deformation in the Lower Yangtze region[J].Regional Geology of China,1999,18(1):73-79.
    [8]
    朱日祥,杨振宇,吴汉宁,等.中国主要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):1-16. ZHU Rixiang,YANG Zhenyu,WU Hanning,et al.Paleomagnetic constraints on the tectonic history of the major blocks of China during the Phanerozoic[J].Science in China(Series D:Earth Sciences),1998,41(S2):1-19.
    [9]
    黄宝春,周姚秀,朱日祥.从古地磁研究看中国大陆形成与演化过程[J].地学前缘,2008,15(3):348-359. HUANG Baochun,ZHOU Yaoxiu,ZHU Rixiang.Discussions on Phanerozoic evolution and formation of continental China,based on paleomagnetic studies[J].Earth Science Frontiers,2008,15(3):348-359.
    [10]
    梅廉夫,戴少武,沈传波,等.中、下扬子区中、新生代陆内对冲带的形成及解体[J].地质科技情报,2008,27(4):1-7. MEI Lianfu,DAI Shaowu,SHEN Chuanbo,et al.Formation and disintegration of Mesozoic-Cenozoic intra-continental ramp zone in Middle and Lower Yangtze region[J].Geological Science and Technology Information,2008,27(4):1-7.
    [11]
    李海滨,贾东,武龙,等.下扬子地区中-新生代的挤压变形与伸展改造及其油气勘探意义[J].岩石学报,2011,27(3):770-778. LI Haibin,JIA Dong,WU Long,et al.The Mesozoic-Cenozoic compressional deformation,extensional modification and their significance for hydrocarbon exploration in Lower Yangtze region[J].Acta Petrologica Sinica,2011,27(3):770-778.
    [12]
    徐曦,杨风丽,赵文芳.下扬子区海相中、古生界上油气成藏组合特征分析[J].海洋石油,2011,31(4):48-53. XU Xi,YANG Fengli,ZHAO Wenfang.Analysis of characteristics of upper hydrocarbon play of Mesozoic-Paleozoic marine group,Lower Yangtze region[J].Offshore Oil,2011,31(4):48-53.
    [13]
    REN Jianye,TAMAKI K,LI Sitian,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J].Tectonophysics,2002,344(3-4):175-205.
    [14]
    舒良树,王博,王良书,等.苏北盆地晚白垩世-新近纪原型盆地分析[J].高校地质学报,2005,11(4):534-543. SHU Liangshu,WANG Bo,WANG Liangshu,et al.Analysis of Northern Jiangsu Prototype Basin from Late Cretaceous to Neogene[J].Geological Journal of China Universities,2005,11(4):534-543.
    [15]
    万天丰,郝天珧.黄海新生代构造及油气勘探前景[J].现代地质,2009,23(3):385-393. WAN Tianfeng,HAO Tianyao.Cenozoic tectonics of the Yellow Sea and its oil-gas exploration[J].Geoscience,2009,23(3):385-393.
    [16]
    梁兴,叶舟,吴根耀,等.鄱阳盆地构造-沉积特征及其演化史[J].地质科学,2006,41(3):404-429. LIANG Xing,YE Zhou,WU Genyao,et al.Sedimento-tectonic features and geological evolution of the Poyang Basin[J].Chinese Journal of Geology,2006,41(3):404-429.
    [17]
    张义楷.望江-潜山盆地形成演化与含油气系统研究[D].西安:西北大学,2003. ZHANG Yikai.Foramtion-evolution and petroleum system of the Wangjiang-Qianshan basin[D].Xi'an:Northwest Universtiy,2003.
    [18]
    安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1987. Anhui Geology and Mineral Bureau.Bulletin of the Anhui regional geology[M].Beijing:Geological Publishing House,1987.
    [19]
    朱光,宋传中,王道轩,等.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义[J].中国科学(D辑),2001,31(3):250-256. ZHU Guang,SONG Chuanzhong,WANG Daoxuan,et al.Studies on 40Ar/39Ar thermochronology of strike-slip time of the Tan-Lu fault zone and their tectonic implications[J].Science in China (Series D:Earth Sciences),2001,44(11):1002-1009.
    [20]
    张渝昌.江南-雪峰地区的层滑作用及多期复合构造[M].北京:地质出版社,1993. ZHANG Yuchang.Layer-sliding action and multiphase composite structures in the Jiangnan-Xuefeng region[M].Beijing:Geological Publishing House,1993.
    [21]
    侯明金.江南隆起带(安徽部分)燕山晚期岩浆活动与深部过程[D].合肥:合肥工业大学,2005. HOU Mingjin.The magmatic activities and its deepth process of the later Yanshannian granitoids in the Jiangnan uplift in the area of Anhui province[D].Hefei:Hefei University of Techno-logy,2005.
    [22]
    徐菲.潜山盆地沉积特征及其对郯庐断裂带的构造响应[D].合肥:合肥工业大学,2009. XU Fei.The sedimentary features of Qianshan Basin and the structure response to Tan-Lu fault zone[D].Hefei:Hefei University of Technology,2009.
    [23]
    袁政文.下扬子北缘前陆盆地形成演化与油气赋存条件[D].北京:中国科学院地质与地球物理研究所,2004. YUAN Zhengwen.Formation and evolution of foreland basin on the northern margin of the lower reach of the Yangtze River and its oil-gas occurrence[D].Beijing:Institute of Geology and Geophysics,2004.
    [24]
    苏浙皖闽油气区石油地质志编写组.中国石油地质志(卷8)[M].北京:石油工业出版社,1992. Su-Zhe-Wan Editorial Committee.Petroleum geology of China Vol. 8[M].Bejing:Petroleum Industry Press,1992.
    [25]
    吴跃东.大别造山带东南缘中新生代盆地沉积构造演化[D].成都:成都理工大学,2009. WU Yuedong.Sedimentary structural evolution of Mesozoic-Cenozoic basin on southeastern margin of Dabie orogenic belt[D].Chengdu:Chengdu University of Technology,2009.
    [26]
    唐永成,吴言昌,储国正,等.安徽沿江地区铜金多金属矿床地质[M].北京:地质出版社,1998. TANG Yongcheng,WU Yanchang,CHU Guozheng,et al.Copper-gold polymetalic ore deposit geology in the Yangjiang area,Anhui[M].Beijing:Geological Publishing House,1998.
    [27]
    胡德昭,徐鸣洁,黄钟谨.安徽无为盆地平衡地质剖面研究[J].高校地质学报,1996,2(4):72-77. HU Dezhao,XU Mingjie,HUANG Zhongjin.A study on the balanced cross section of Wuwei Basin,Anhui province[J].Geological Journal of China Universities,1996,2(4):72-77.
    [28]
    斯春松,温祥泉.苏皖南地区地质-地球物理综合解释方法探讨:以无为盆地为例[J].海相油气地质,1999,4(2):43-49. SI Chunsong,WEN Xiangquan.A discussion of method of the geology-geophysics integrated interpration method[J].Marine Origin Petroleum Geology,1999,4(2):43-49.
    [29]
    郭念发,姚柏平,吴群.安徽无为盆地油气地质条件评价[J].安徽地质,1999,9(4):289-294. GUO Nianfa,YAO Baiping,WU Qun.The appraisal of oil and gas geological conditions of the Wuwei Basin,Anhui[J].Geo-logy of Anhui,1999,9(4):289-294.
    [30]
    蔡希源.中国油气区反转构造[M].北京:石油工业出版社,2001. CAI Xiyuan.Reverse structure in China petroleum provinces[M].Beijing:Petroleum Industry Press,2001.
    [31]
    朱立华.下扬子地区盆地构造演化及其对油气的控制[D].南京:南京大学,2001. ZHU Lihua.The tectonic evolution of basin and its controlling on oil and gas in the Lower Yangtze area[D].Nanjing:Nanjing University,2001.
    [32]
    沈淑鑫,李一泉,崔键,等.下扬子黄桥地区构造特征及其与油气的关系[J].高校地质学报,2015,21(3):538-552. SHEN Shuxin,LI Yiquan,CUI Jian,et al.The structural characteristics in Huangqiao area in the Lower Yangtze region and its relationship to oil and gas accumulation[J].Geological Journal of China Universities,2015,21(3):538-552.
    [33]
    吕庆田,侯增谦,赵金花,等.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态[J].中国科学(D辑),2003,33(5):442-449. LV Qingtian,HOU Zengqian,ZHAO Jinhua,et al.Deep seismic reflection profiling revealing the complex crustal structure of the Tongling ore district[J].Science in China (Series D:Earth Sciences),2004,47(3):193-200.
    [34]
    胡连英.溧阳地震与茅东断裂带[M].北京:地震出版社,1997. HU Lianying.The Liyang earthquakes and the eastern fault zone of Maodong[M].Beijing:Seismological Press,1997.
    [35]
    盛勇,李仁和,廖圣柱,等.宣郎地区基底构造特征[J].地质科学,2014,49(2):394-404. SHENG Yong,LI Renhe,LIAO Shengzhu,et al.Characteristics of the basement structure in Xuancheng-Langxi area[J].Chinese Journal of Geology,2014,49(2):394-404.
    [36]
    练铭祥,薛冰,杨盛良.苏北新生代盆地断陷和坳陷的形成机理[J].石油实验地质,2001,23(3):256-260. LIAN Mingxiang,XUE Bing,YANG Shengliang.Formation mechanism of depressions and rifts in the Cenozoic basin of north Jiangsu province[J].Petroleum Geology & Experiment,2001,23(3):256-260.
    [37]
    白云风,程日辉,孔庆莹,等.下扬子地区晚白垩世浦口期沉积古地理及地质背景[J].吉林大学学报(地球科学版),2007,37(4):684-689. BAI Yunfeng,CHENG Rihui,KONG Qingying,et al.Sedimentary paleogeography and geological background in the Pukou stage of Late Cretaceous period in the Lower Yangtze area[J].Journal of Jilin University(Earth Science Edition),2007,37(4):684-689.
    [38]
    能源,杨桥,张克鑫,等.苏北盆地高邮凹陷晚白垩世-新生代构造沉降史分析与构造演化[J].沉积与特提斯地质,2009,29(2):25-32. NENG Yuan,YANG Qiao,ZHANG Kexin,et al.Tectonic subsidence and evolution of the Gaoyou Depression in Northern Jiangsu Basin during the Late Cretaceous to the Cenozoic[J].Sedimentary Geology and Tethyan Geology,2009,29(2):25-32.
    [39]
    陈安定.苏北盆地构造特征及箕状断陷形成机理[J].石油与天然气地质,2010,31(2):140-150. CHEN Anding.Tectonic features of the Subei Basin and the forming mechanism of its dustpan-shaped fault depression[J].Oil & Gas Geology,2010,31(2):140-150.
    [40]
    柯光明.苏皖地区中、新生代层序地层研究及其在油气勘探开发中的应用[D].成都:成都理工大学,2007. KE Guangming.Study of sequence stratigraphy and its application for oil and gas exploration and development in Late Mesozoic and Cenozoic of Jiangsu and Anhui area[D].Chengdu:Chengdu University of Technology,2007.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1767) PDF downloads(404) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return