地球科学进展 ›› 2000, Vol. 15 ›› Issue (6): 661 -665. doi: 10.11867/j.issn.1001-8166.2000.06.0661

综述与评述 上一篇    下一篇

沉积盆地构造热演化模拟的研究进展
何丽娟   
  1. 中国科学院地质与地球物理研究所,北京 100029
  • 收稿日期:2000-02-28 修回日期:2000-04-24 出版日期:2000-12-01
  • 通讯作者: 何丽娟(1968-),女,河南省开封市人,助研,主要从事盆地构造热演化模拟方面的工作。
  • 基金资助:

    国家基础研究发展规划项目“中国典型叠合盆地深部热体制转换与热史反演”(编号:G1999043302);国家自然科学基金项目“多期拉伸盆地构造热演化模拟的运动学-流变学研究”(编号:49804004)和中国科学院资源与生态环境研究重点项目“沉积盆地系统及其动力学基础研究”(编号:KZ952-S1-428)联合资助。

ADVANCE IN TECTONO-THERMAL MODELLING OF SEDIMENTARY BASINS

HE Li-juan   

  1. Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China
  • Received:2000-02-28 Revised:2000-04-24 Online:2000-12-01 Published:2000-12-01

沉积盆地构造热演化模拟建立在盆地成因的地质地球物理模型基础之上,其中包括运动学模型、运动学—流变学模型和动力学模型。运动学模型在预测盆地热流演化方面具有优势,但在预测构造沉降等几何形态方面存在一定的缺陷;运动学—流变学模型的优势在于构造演化模拟,在热演化方面类似于运动学模型;动力学模型蕴含着潜在的巨大优势,只是目前还存在一些阻碍因素。构造热演化正演模型的进一步完善及正、反演模型的匹配将是未来构造热演化模拟的发展趋势。

Tectono-thermal modeling is based on the geological-geophysical models of basin formation,which include kinematic model, kinematic-rheological model and dynamic model. Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry; Kinematic-rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction;Dynamic models contain latent advantages and also some obstacles in tectono-thermal modeling. Future study should put emphasis on further improvement of tectono-thermal models and its matching with reverse models.

中图分类号: 

[1]Fernandez M, Ranalli G. The role of rheology in extensional basin formation modelling[J]. Tectonophysics, 1998, 282:129~145.
[2]McKenzie D P. Some remarks on the development of sedimentary basins[J]. Earth Planet Sci Lett, 1978, 40:25~32.
[3]Jarvis G T, McKenzie D P. Sedimentary basin formation with finite extension rates[J]. Earth Planet Sci Lett, 1980, 48:42~52.
[4]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, 51:343~361.
[5]Hellinger S J, Sclater J G. Some commonts on two-layer extension models for the evolution of sedimentary basins[J].J Geophys Res, 1983, 88:8 251~8 269.
[6]Rowley D B, Sahagian D. Depth-dependent stretching: a different approach[J]. Geology, 1986, 14:32~35.
[7]Egan S S. The flexural isostatic response of the lithosphere to extensional tectonics[J]. Tectonophysics, 1992, 202:291~308.
[8]Keen C E, Dehler S A. Stretching and subsidence: rifting of conjugate margins in the North Atlantic region[J]. Tectonics,1993, 12: 1 219~1 229.
[9]何丽娟,熊亮萍,汪集日易.沉积盆地多期拉张模拟中拉张系数的计算[J].科学通报,1995, 40(24):2 261~2 263.
[10]Dehler S A, Keen C E, Rohrt K M. Tectonic and thermal evolution of Queen Charlotte basin: lithospheric deformation and subsidence models[J]. Basin Research, 1997, 9: 243~261.
[11]Lin Changsong, Li Sitian, Zhang Qiming,et al. Subsidence and stretching of some Mesozoic-Cenozoic rift basins in East China[A]. Proceedings of the 30th International Geological Congress[C]. 1996. 176~196.
[12]何丽娟,熊亮萍,汪集日易.拉张盆地多期构造热演化模拟中的影响因素[J].地质科学,1998,33(2):125~131.
[13]何丽娟.辽河盆地新生代多期构造热演化模拟[J].地球物理学报,1999,42(1):75~82.
[14]何丽娟,熊亮萍,汪集日易,等.莺歌海盆地构造热演化模拟研究[J].中国科学(D), 2000, 30(4):415~419.
[15]Braun J, Beaumont C. A physical explanation of the relation between the flank uplifts and the breakup unconformity at rifted continental margins[J]. Geology, 1989, 17:760~764.
[16]Weissel J K, Karner G D. Flexural uplift of rift flanks due to mechanical unloading of the lithosphere during extension[J].J Geophys Res, 1989, 94: 919~950.
[17]Karner G D, Egan S S, Weissel J K. Modeling the tectonic development of the Tucano and Sergipe-Alagoas rift basins,Brazi[J]. Tectonophysics, 1992, 215:133~160.
[18]Kusznir N J, Ziegler P A. The mechanics of continental extension and sedimentary basin formation: A simple-shear/puer-shear flexureal cantilever model[J]. Tectonophysics,1992, 215:117~131.
[19]Kooi H, Cloetingh S, Burrus J. Lithospheric necking and regional isostasy at extensional basins, 1: Subsidence and gravity modeling with an application to the Gulf of Lions Margins (S E France) [J]. J Geophys Res, 1992, 97:17553~19 572.
[20]Bassi G, Keen C E, Potter P. Contrasting styles of rifting:Models and examples from the eastern Canadian margin[J].Tectonics, 1993, 12:639~655.
[21]Janssen M E, Torn M, Cloetingh S,et al. Pliocene uplift of the Eastern Iberian margin: inferences from quantitative modeling of the Valencia Trough[J]. Earth Planet Sci Lett,1993, 199:585~597.
[22]Pedersen T. Some remarks on lithospheric forces and decompression magmatism[J]. Tectonopyhsics, 1994,240:11~19.
[23]Spadini G, Cloetingh S, Bertotti G. Thermo-mechanical modeling of the Tyrrhenian Sea: Lithospheric necking and kinematics of rifts[J]. Tectonics, 1995, 14(3): 629~644.
[24]Stockmal G S, Beaumont C, Boutelier R. Geodynamics. models of convergen margin tectonics: the transition from rifted margin to overthrust belt and consequences for foreland basin development[J]. AAPG Bull, 1986, 70:181~190.
[25]Watts A B. Lithospheric flexure due to prograding loads:implications for the origin of offlap/onlap patterns in sedimentary basins[J]. Basin Research, 1989, 2:133~144.
[26]Beaumont C, Quinlan G M, Stockmal G S. The evolution of the western interior basin, cause, consequences and unsolved problems. Evolution of the western interior basin [J].Geological Association of Canada Special Paper, 1993, 39:97~117.
[27]Johnson D D, Beaumont C. Preliminary results from a platform kinematic model of orogen evolution, surface processes and the development of classic foreland stratigraphy [A]. Stratigraphic Evolution of Foreland Basins[C], SEPM Special Publication 52, 1995. 3~24.
[28]林场松,刘景彦,张燕梅.沉积盆地动力学与模拟研究[J].地学前缘,1998, 5(增刊):119~125.
[29]Egan S S, Urquhart J M. Numerical modelling of lithosphere shorting: application to the Laramide orogenic province,western USA[J]. Tectonophysics, 1993, 221:385~411.
[30]Hodgetts D, Egan S S, Williams G D. Flexural modelling of continental lithosphere deformation: a comparison of 2D and 3D techniques[J]. Tectonophysics, 1998, 294:1~20.
[31]Hendrie D B, Kusznir N J, Hunter R H. Jurassic extension estimates for the North Sea“triple junction”from flexural backstripping: implications for decompression melting models[J]. Earth Planet Sci Lett, 1993, 116:113~127.

[1] 邓文文, 王荣, 刘正文, 郑文秀, 张晨雪. 模型揭示的浅水湖泊稳态转换影响因素分析[J]. 地球科学进展, 2021, 36(1): 83-94.
[2] 夏少红, 曹敬贺, 万奎元, 范朝焰, 孙金龙. OBS广角地震探测在海洋沉积盆地研究中的作用[J]. 地球科学进展, 2016, 31(11): 1111-1124.
[3] 陆志翔, 肖洪浪, 邹松兵, 任娟, 张志强. 黑河流域近两千年人—水—生态演变研究进展[J]. 地球科学进展, 2015, 30(3): 396-406.
[4] 陈汉林, 陈沈强, 林秀斌. 帕米尔弧形构造带新生代构造演化研究进展[J]. 地球科学进展, 2014, 29(8): 890-902.
[5] 吴增茂;谢红琴;张志南;万小芳. 海洋生态预报的复杂性与研究方法的讨论[J]. 地球科学进展, 2004, 19(1): 81-086.
[6] 帅燕华,邹艳荣,彭平安. 天然气甲烷碳同位素动力学模型与地质应用新进展[J]. 地球科学进展, 2003, 18(3): 405-411.
[7] 李祥辉,包向农. 海平面变化成因及其盆地响应[J]. 地球科学进展, 2000, 15(1): 71-75.
[8] 吴增茂;俞光耀. 海洋生态系统动力学模型的基本特征及其研究进展[J]. 地球科学进展, 1996, 11(1): 13-18.
[9] 方国庆; 张晓宝. 板块沉积学[J]. 地球科学进展, 1993, 8(4): 80-82.
[10] 周中毅,潘长春,闵育顺,施继锡,王庆隆. 沉积盆地古地温测定方法及应用[J]. 地球科学进展, 1991, 6(5): 44-45.
[11] 周庆凡. 国外沉积盆地分析研究的新进展[J]. 地球科学进展, 1991, 6(4): 45-48.
阅读次数
全文


摘要