ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
与陆-陆碰撞作用相关的盆-山构造数值模拟
  
关键词:continent-continent collision  intracontinental subduction zone  basin-range tectonics  numerical modeling  tectonic interface  displacement
基金项目:国家“305”项目(编号:96-915-06-04); 国家自然科学基金项目(编号:19972072); 国土资源部大陆动力学开放实验室项目(编号:9812)
作者单位
崔军文 中国地质科学院地质研究所北京100037 
史金松 河海大学江苏南京210024 
李朋武 中国地质科学院地质研究所北京100037 
张晓卫 中国地质科学院地质研究所北京100037 
郭宪璞 中国地质科学院地质研究所北京100037 
丁孝忠 中国地质科学院地质研究所北京100037 
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摘要:
Numerical Modeling of Basin-Range Tectonics Related to Continent-Continent Collision
      Continent-continent collision is the most important driving mechanism for various geological processes in the continental lithosphere. The recognition and determination of continent-continent collision, especially its four-dimensional temporal and spatial evolution, is a subject which has long aroused concern and research interest in geological communities. Continent-continent collision mainly finds expression in strong underthrusting (subduction) of the underlying block along an intracontinental subduction zone and continuous obduction (thrusting propagation) of the overlying block along the intracontinental subduction zone, the formation of a basin-range tectonic framework in a direction perpendicular to the subduction zone and the flexure and disruption of the Moho. On the basis of numerical modeling, the authors discuss in detail the couplings between various quantities and rates of displacement caused by basin subsidence, mountain uplift and Moho updoming and downflexure during obduction (thrusting propagation) and subduction and the migration pattern of basin centers. They are probably indications or criteria for judgment or determination of continent-continent collision.
CUI Jun-wen,SHI Jin-song,LI Peng-wu,ZHANG Xiao-wei,GUO Xian-pu,DING Xiao-zhong.2006.Numerical Modeling of Basin-Range Tectonics Related to Continent-Continent Collision[J].Acta Geoscientica Sinica,27(1):13-24.
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