沉积盆地构造热演化模拟的研究进展

doi:10.11867/j.issn.1001-8166.2000.06.0661

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

沉积盆地构造热演化模拟的研究进展

何丽娟

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

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

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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。

关键词: 沉积盆地, 构造热演化模拟, 运动学模型, 运动学—流变学模型, 动力学模型

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.

Key words: Sedimentary basins, Tectono-thermal modeling, Kinematic model, Kinematic-rheological model, Dynamic model.

中图分类号:

P554

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