收稿日期: 2008-10-06
修回日期: 2009-02-27
网络出版日期: 2009-12-12
基金资助
国家自然科学基金项目（40576027）
Numerical Models of the Tectono-Thermal Evolution of Rift Basins and Their Applications to the Northern South China Sea
Received date: 2008-10-06
Revised date: 2009-02-27
Online published: 2009-12-12
Supported by
国家自然科学基金项目（40576027）
廖杰 , 周蒂 , 赵中贤 . 裂谷盆地构造热演化的数值模型及在南海北部的应用[J]. 热带海洋学报, 2009 , 28(6) : 41 -51 . DOI: 10.11978/j.issn.1009-5470.2009.06.041
Numerical models are the basis for quantitative modeling of the tectono-thermal evolution of sedimentary basins. Due to the importance of rift basins in scientific research and petroleum exploration, extensive studies have been devoted to building numerical models for rift basins. This paper summarizes the models that have great influence or play an important role in the study of the passive continental margin of the South China Sea, including the most fundamental model of McKenzie, and the models of finite-rate stretching, simple shear stretching, flexural cantilever stretching, depth-dependent stretching, and multiphase stretching. Special emphasis was placed on their basic assumptions, application conditions, and numerical formulations for the geothermal field and basin subsidence. The similarities, differences, and correlations of these models were expounded. Finally, the applications of the models in studying the rift basins in the northern South China Sea were briefed, which may help to advance our understanding of the methods and applications of the numerical models.
[1] 何丽娟,汪集旸. 沉积盆地构造热演化研究进展:回顾与展望[J]. 地球物理学进展, 2007 (4): 1215-1219.
[2] MCKENZIE D P. Some remarks on the development of sedimentary basins[J]. Earth Planet Sci Lett, 1978: 25-32.
[3]ALLEN P A,ALLEN J R. Basin analysis: principles and applications[M]. London: Blackwell Scientific Publications, 1990.
[4] BOCCALETTI M, HORVATH F, LODDO M, et al. The Tyrrhenian and Pannonian Basins: a comparison of two Mediterranean interarc basin[J]. Tectonophysics, 1976 (45).
[5] JARVIS J T,MCKENZIE D P. Sedimentary basin formation with finite extension rates[J]. Earth Planet Sci Lett, 1980: 42-52.
[6] COCHRAN J R. Effects of finite rifting times on the development of sedimentary basins[J]. Earth Planet Sci Lett, 1983: 289-302.
[7] WERNICKE B. Low-angle normal faults in the basin and range province:nappe tectonics in an extending orogen[J]. Nature, 1981: 645-647.
[8] WERNICKE B. Uniform-sense normal simple-shear of the continental lithosphere[J]. Can J Earth Sci, 1985: 108-125.
[[9] KUSZNIR N J,MATTHEWS D H. Deep seismic reflections and the deformational mechanics of the continental lithosphere[J]. J.Petrol, Special Lithosphere Issue,1988: 66-87.
[10]KUSZNIR N J, MARSDEN G,EGAN S S: A flexural-cantilever simple-shear/pure-shear model of continental lithosphere extension:applications to the Jeanne d'Arc Basin,Grand Banks and Viking Graben,North Sea, ROBERTS A M, YIELDING G, KARMER D, et al., editor, The Geometry of Normal Faults: Geological Society Special Publication, 1991: 41-60.
[11] KUSZNIR N J,ZIEGLER P A. The mechanics of continental extension and sedimentary basin formation:A simple-shear/pure-shear flexural cantilever model[J]. Tectonophysics, 1992: 117-131.
[12]TURCOTTE D L,SCHUBERT G. Geodynamics[M]. Cambridge: Cambridge University Press, 2002.
[13] ROYDEN L,KEEN C E. Rifting processes and thermal evolution of the continental margin of eastern Canada determined from subsidence curves[J]. Earth Planet Sci Lett, 1980: 343~361.
[14] ROWLEY D B,SAHAGIAN D. Depth-dependent stretching: A different approach[J]. Geology, 1986: 32-35.
[15]DAVIS M,KUSZNIR N J. Depth-dependent lithospheric stretching at rifted continental margins. Proceedings of national science foundation rifted margins theoretical institute. New York: Columbia University Press, 2004: 92-137.
[16] WALSH J, WATTERSON J,YIELDING G. The importance of small scale faulting in regional extension[J]. Nature, 1991: 391-393.
[17] ROBERTS A M, KUSZNIR N J, YIEDLING G, et al. 2D flexural backstripping of extensional basins: the need for a sideways glance[J]. Petrol Geosci, 1998: 327-338.
[18] ROBERTS A M, YIELDING G, KUSZNIR N J, et al. Quantitative analysis of Triassic extension in the northern Viking Graben[J]. Geol Soc London, 1995 (1): 15-26.
[19]BADLEY GEOSCIENCE LTD. Software products. 2004-2007.
[20] LIN CHANGSONG, ZHANG YINGMEI, LI SITIAN, et al. Quantitative modelling of multiphase lithosphere stretching and deep thermal history of some tertiary rift basins in Eastern China[J]. Acta Geol Sin, 2002 (3): 324－330.
[21] 林畅松, 张燕梅, 李思田, et al. 中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型[J]. 地球科学－中国地质大学学报, 2004 (5): 583－588.
[22]陈艺中: 南海北部陆缘二地学断面的地质、地球物理特征, 姚伯初,曾维军, editor, 中美合作调研南海地质专报, 武汉: 中国地质大学出版社, 1994: 117-134.
[23] SCLATER J G,CHRISTIE P A F. Continental stretching: An explanation of the post-Mid-Cretaceous subsidence of the central North Sea basin[J]. J Geophys Res, 1980 (B7): 3711-3739.
[24] CLIFT P,LIN J. Preferential mantle lithospheric extension under the South China margin[J]. Mar Petrol Geol, 2001 (8): 929-945.
[25] CLIFT P, LIN J,Barckhausen U. Evidence of low flexural rigidity and low viscosity lower continental crust during continental break-up in the South China Sea[J]. Mar Petrol Geol, 2002 (8): 951-970.
[26] SHI XIAOBIN, BUROV E, LEROY S, et al. Intrusion and its implication for subsidence: A case from the Baiyun Sag, on the northern margin of the South China Sea[J]. Tectonophysics, 2005: 117-134.
[27]陈长民, 施和生, 许仕策, et al. 珠江口盆地 (东部) 第三系油气藏形成条件[M]. 北京: 科学出版社, 2003.
[28] RU KE,PIGOTT J D. Episodic rifting and subsidence in the South China Sea[J]. AAPG Bulletin, 1986: 1136-1155.
[29] ZHOU DI, SUN ZHEN, LIAO JIE, et al. Filling history and post-breakup acceleration of sedimentation in the Baiyun Sag, deep-water northern South China Sea[J]. Earth Sci-J China University Geosci, 2009 (1): 160-171.
[30] XIE XINONG, DIETMAR R, LI S, et al. Origin of anomalous subsidence along the Northern South China Sea margin and its relationship to dynamic topography[J]. Mar Petrol Geol, 2006: 745-765.
[31] HE LIJUAN, XIONG LIANGPING, WANG JIYANG, et al. Tectono-thermal modeling of the Yinggehai Basin, South China Sea[J]. Sci China Ser D-Earth Sci, 2001 (1): 7-13.
[32] 何丽娟, 熊亮萍, 汪集旸, et al. 沉积盆地多次拉张模拟中拉张系数的计算[J]. 科学通报, 1995 (24): 2261－2263.
何丽娟. 拉张盆地的热演化模拟研究-以南海盆地和辽河盆地为例[D]. 中国科学院地质研究所, 北京, 1996: 1-84.
[34] 何丽娟, 熊亮萍,汪集旸. 拉张盆地构造热演化模拟的影响因素[J]. 地质科学, 1998 (2): 222-227.
[35]KUSZNIR N J,KARNER G D: Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland and Iberia margins, Karner G D, Manatschal G,Pinheiro L M, editor, Imaging, mapping and modelling continental lithosphere extension and breakup, London: Geological Society, Special Publication, 2007: 389-419.
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