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《Resources and Environment in the Yangtze Basin》 2003-05
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BASIN-RANGE SYSTEM EVOLUTION OF QINLING-DABIE OROGENIC BELT AND ITS EFFECTS ON REGIONAL ENVIRONMENT

HU Bao-qing 1,2 ,LIU Shun-sheng 3 ,WANG Shi-jie 1 ( 1.National Laboratory of Environmental Geochemistry,Geochemistry Institute of The Chinese Academy of Sciences,Guiyang550002,China;2.Department of Geography,Guangxi Teacher's College,Nanning530001,China;3.Guangzhou Institute of Geochemistry,The Chinese Academy of Sciences,Guangzhou510640,China )  
As the structural body in relation to temporal-spatial evolution and tectonic dynamic system,the orogenic belt and basin are not only dependent of one another in space,but closely related in terms of infrastructure,matter transference and dynamic mechanisms.By using apatite fission-track method ,the authors firstly analyzed the uplift and exhumation ratio of Qinling-Dabie orogenic belt,and by using tectonically deformed combination analysis and tectonic-thermal simulation the main geological occurrences were also illustrated.It is found that there must have had multi-phase differential uplift and exhumation phenomena in Qinling-Dabie orogenic belt during Mesozoic-Cenozoic.Then,the regional evolution pattern of qualitative and quantitative denudation process is resulted during post-orogenic period.On the bases of summarizing evolution process of basin-range system in Qinling-Dabie orogenic belt during the Mesozoic-Cenozoic and its effects on regional environment,the influence of evolution process on geomorphologic landscapes change,water system vicissitude,eco-environment succession and drainage basin system evolution was discussed.
【Fund】: 中国科学院院长基金特别支助项目“大别造山带裂变径迹年代及构造热历史研究”(1999)资助.
【CateGory Index】: P542.2
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