XU Han-lin, SHEN Yang, DING Xiao, XU Jia-wei. STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(4): 285-290. doi: 10.11781/sysydz199904285
Citation: XU Han-lin, SHEN Yang, DING Xiao, XU Jia-wei. STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(4): 285-290. doi: 10.11781/sysydz199904285

STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA

doi: 10.11781/sysydz199904285
  • Received Date: 1998-04-01
  • Rev Recd Date: 1999-08-19
  • Publish Date: 1999-10-28
  • Basin and range structure developed during the Meso-Cenozoic period in Southeast China was controlled by those pre-existed fault systems.There are three fault systems in the area with NNE-NE, nearly E-W, NW strikes.Based on the characteristics of the basins, there are three types of basins in the area: graben, listric faults and transform-extension.The characteristics of the basin and range province in Southeast China is shown by longitudinal blocks in S-N and cross zones in E-W.Formation of basin and range province in Southeast China was mainly resulted from geodynamic evolution of west marginal-Pacific tectonic domain, and from collision and squeezing of Indian plate with Euro-Asian continent.

     

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  • [1]
    徐嘉炜.郯城-庐江平移断裂系统[A].构造地质学论丛[C],第3期.北京:地质出版社,1984.
    [2]
    Xu JW,Zhu G,Tong WX,Cui KR,Liu Q.Formation and evolution of the Tancheng-Lujiang wrench fault system: a major shear system to the Northwest of the Pacific Ocean[J].Tectonophysics,1987,134:273~310.
    [3]
    万天丰,朱鸿.白垩纪到早始新世中国构造应力场及其环境[A].中国及邻区构造古地理及古生物地理[C].武汉:中国地质大学出版社,1990.245~261.
    [4]
    Gilder S A, R S Coe, H Wu, G D Kuang, X X Zhao, QWu, X Z Tang.Cretaceous and Tertiary Paleomagnetic Results from Southeast China and their Tectonic Implications[M].EPSL(in Press),1993.
    [5]
    顾心如.江西吉泰盆地晚白垩世红层古地磁结果的大地构造含义[J].江西地质,1990,4(4):431~443.
    [6]
    沈修志,等.华北南部盆地逆冲推复构造特征与煤成气关系[J].南京大学学报(地球科学),1993,5(2).
    [7]
    刘和甫,吴振明,汤良杰,高金喜.亚洲大陆中新生代裂谷系演化及构造分析[A].国际交流地质学术论文集(2)[C].北京:地质出版社,1985.
    [8]
    Wernicke B, Burchfiel B C.Modes of extensional tectonics[J].Journal of Structural Geology, 1982,4(2):105 ~115.
    [9]
    Xu J W, Tong W X.Major characteristics of the epi-continental arcs of East Asia and their tectonic significance[J].J.Southeast Asian Earth Sciences,1988,2(1):23~ 33.
    [10]
    王良本,施央申.油气盆地地热研究[M].南京:南京大学出版社,1989.
    [11]
    Lister G S,Davis G A.The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region, U.S.A.[J].Jour.Struct.Geology,1989,11:65~94.
    [12]
    陈焕疆.论板块大地构造与油气盆地分析[M].上海:同济大学出版社,1990.
    [13]
    Xu J W, Tong W X, Zhu G, Lin S F,Ma G F.An outline of the pre-Jurassic tectonic framework in East Asia[J].J.Southeast Asian Earth Sciences, 1990,3(1~4):19~45.
    [14]
    徐嘉炜,朱光,马国锋.东亚大陆边缘演化的若干认识[A].亚洲的增生[C].北京:地震出版社,1993.
    [15]
    朱夏.论中国含油气盆地构造[M].北京:石油工业出版社,1956.
    [16]
    郭福祥.中国东部及邻区中新生代盆地-山脉系的地质构造特征及形成[J].云南地质,1989,8(2).
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