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LI Ji-liang, XIAO Wen-jiao, YAN Zhen. Basin-Range Coupling and Its Sedimentation[J]. Acta Sedimentologica Sinica, 2003, 21(1): 52-60.
Citation: LI Ji-liang, XIAO Wen-jiao, YAN Zhen. Basin-Range Coupling and Its Sedimentation[J]. Acta Sedimentologica Sinica, 2003, 21(1): 52-60.

Basin-Range Coupling and Its Sedimentation

  • Received Date: 2002-12-26
  • Rev Recd Date: 2003-01-10
  • Publish Date: 2003-03-10
  • Basin-Rang coupling is an important geological phenomenon. According to the dynamic mechanism, six types of basin-range coupling can be divided: extensional, compressive, transextensive, transpressive, vertical stress deduced and impact. In this paper, the structural characteristics and typical sedimentation of each types of basin-range coupling are elaborated.
  • [1] [1]Cloetingh S, Sassi W, Hoevath F. The origin of Sedimentary Ba sins: Inferences from Quantative Modelling and Basin Analysis[J]. Tectonophysi cs, 1993, 226: 1~518

    [2]Cloetingh S, Eldholm O, Larsen B T, Gabrielsen R, Sassi W. Dynamics of Extensional Basin Formation[J]. Tectonophysics, 1994, 240: 1~341

    [3]Cloetingh S, D'Argenio B, Catalano R, Horvath F, Sassi W. Interplay of Extension and Compression in Basin Formation[J]. Tectonophysics, 1995, 252: 1~ 484

    [4]Cloetingh S, Ben Avraham Z, Sassi W, Horvath F. Dynamics of Extensional Basins and inversion Tectonics[J]. Tectonophysics, 1996, 266: 1~523

    [5]Cloetingh S, Fernandez M, Munoz J A, Sassi W, Horvath F. Structural Con trols on Sedimentary Basin Formation[J]. Tectonophysics, 1997, 282: 1~442

    [6]Cloetingh S, Bordreel L O, Larsen B T, Heinesen M, Mortensen L. Tecton ics of Sedimentary Basin Formation[J]. Tectonophysics, 1998, 300: 1~387

    [7]Cloetingh S, D'Argenio B, Catalano R, Horvath F, Sassi W. Basin Dynamic s and Basin Fill: Models and Constrains, Part 1[J].Tectonophysics, 1999, 315:1 ~384

    [8]Cloetingh S, Podlachikov Y. Basin Origin and Crustal Structure[J]. Te ctonophysics, 2000, 320:1~432

    [9]Cloetingh S, Marzo M, Munoz J A, Verges. Tectonics of Sedimentary Basin s: from Crustal Structure to Basin Fill[J]. Tectonophysics, 2002, 340:1~135

    [10]Busby C J, Ingersoll R V. Tectonics of Sedimentary Basins[M]. Blackwell Sc ience Inc., Cambridge, Massachusett. 1995. 578

    [11]Mascle A, Puigdefabregas C, Luterbacher H P, Fernandez M. Cenozoic Foreland Basins of Western Europe[M]. Geological Society Special Publication, London, 1 998, (134):427

    [12]Franke W, Haak V, Oncken O, Tanner D. Orogenic Processes: Quantification and Modelling ijn the Variscan Belt[M]. Published by the Geological Society, Lond on. 2000. 459

    [13]Olier C, Pain C. The Origin of Mountain[M]. Routledge, London and Newyork. 2000. 345
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  • Received:  2002-12-26
  • Revised:  2003-01-10
  • Published:  2003-03-10

Basin-Range Coupling and Its Sedimentation

Abstract: Basin-Rang coupling is an important geological phenomenon. According to the dynamic mechanism, six types of basin-range coupling can be divided: extensional, compressive, transextensive, transpressive, vertical stress deduced and impact. In this paper, the structural characteristics and typical sedimentation of each types of basin-range coupling are elaborated.

LI Ji-liang, XIAO Wen-jiao, YAN Zhen. Basin-Range Coupling and Its Sedimentation[J]. Acta Sedimentologica Sinica, 2003, 21(1): 52-60.
Citation: LI Ji-liang, XIAO Wen-jiao, YAN Zhen. Basin-Range Coupling and Its Sedimentation[J]. Acta Sedimentologica Sinica, 2003, 21(1): 52-60.
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