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《Chinese Journal of Geology》 2005-04
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EXHUMATION AND DENUDATION OF THE DABIE OROGENIC BELT: CONSTRAINTS FROM METAMORPHIC CLASTS OF MESOZOIC SEDIMENTARY ROCKS IN THE SOUTHERN MARGIN OF HEFEI BASIN

Li Shuangying 1 Wang Daoxuan 1 Liu Yin 1 Li Renwei 2 Meng Qingren 2 Yue Shucang 1(1. College of Resources and Environment, Hefei University of Technology, Hefei 230009; 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029)  
The conglomerates, composed of metamorphic detritals, extensively developed in the Mesozoic strata in the south margin of Hefei Basin. The clasts'variety in the strata and sections provided important constraints on the types of source rocks and exhumation and unroofing history of the Dabie orogenic belt. The clasts of conglomerates of Jurassic Sanjianpu and Fanghushan Formations were dominated by metamorphic rocks of greenschist facies and amphibolite facies. The clast associations could match with metamorphic rocks of Foziling and Luzhenguan Groups, which implied that they might be source lands of the Jurassic sediments. The Fuziling and Luzhenguan Groups constituted the basement of the south margin of the basin, so that they had outcropped prior to late period of Early Jurassic (Pliensbachian stage, 195 Ma ago) and suffered erosion. The clasts, occurred in the conglomerates of Early Cretaceous Fenghuangtai, Maotanchang and Zhougongshan Formations, consisted of schist, gneiss, migmatite, eclogite, ultrabasic rock, granite, marble and so on. The clasts'features failed to support that they originated from the UHP terrains preserved in the Dabie orogenic belt, in despite of the eclogite clasts belonging to UHP group. They might belong to a UHP terrain that exhumated to surface prior to Early Cretaceous and suffered erosion, and had disappeared at present. The clasts in Mesozoic strata in the south margin of Hefei Basin lacked a petrographic linkage with the UHP terrains preserved in the Dabie orogenic belt, suggesting that it was in Cenozoic that they came to exhumate and denudate on scale and continue to now. So, three stages for exhumation and denudation history in the Dabie orogenic belt could be distinguished: in prior to Early Jurassic, Late Jurassic-Early Cretaceous and Cenozoic.
【Fund】: 国家重点基础研究发展规划项目(编号:G1999075507)资助。
【CateGory Index】: P542.2;P588.3
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