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Thrusting and Exhumation Processes of a Bounding Mountain Belt: Constraints from Sediment Provenance Analysis of the Hefei Basin
引用本文:LIU Shaofeng,LIU Wencan,Faculty of Geosciences and Resources,China University of Geosciences,Beijing DAI Shaowu,Institute of Exploration and Development,Jianghan Petroleum Administration,Guanghu,Hubei ProvinceHUANG Siji China University of Geosciences,Wuhan and LU Wuyun Anhui Bureau of Geology and Mineral Resources,Hefei. Thrusting and Exhumation Processes of a Bounding Mountain Belt: Constraints from Sediment Provenance Analysis of the Hefei Basin[J]. 《地质学报》英文版, 2001, 75(2): 144-150. DOI: 10.1111/j.1755-6724.2001.tb00516.x
作者姓名:LIU Shaofeng  LIU Wencan  Faculty of Geosciences and Resources  China University of Geosciences  Beijing DAI Shaowu  Institute of Exploration and Development  Jianghan Petroleum Administration  Guanghu  Hubei ProvinceHUANG Siji China University of Geosciences  Wuhan and LU Wuyun Anhui Bureau of Geology and Mineral Resources  Hefei
作者单位:LIU Shaofeng,LIU Wencan,Faculty of Geosciences and Resources,China University of Geosciences,Beijing 100083DAI Shaowu,Institute of Exploration and Development,Jianghan Petroleum Administration,Guanghua 433124,Hubei ProvinceHUANG Siji China University of Geosciences,Wuhan 430074and LU Wuyun Anhui Bureau of Geology and Mineral Resources,Hefei 230091
摘    要:Lithic (or gravel) composition analyses of the Jurassic Sanjianpu Formation and Fenghuangtai Formation in the Hefei basin show that the sediment provenance consists mainly of four kinds of rock units: the basement metamorphic complex, granitic rocks, medium- and low-grade metamorphic rocks, and sandy and muddy sedimentary rocks, which are distributed along the bounding thrust belt. The whole stratigrapnic section can be divided into 2 lithic sequences and 7 subsequences. The regular distribution and changes of lithic fragments and gravels in lithic (or gravel) sequences reflect that the bounding thrust belt of basin has undergone 2 thrusting cycles and 7 thrusting events. Lithic (or gravel) composition analyses of the basin fully reveal that the northern Dabie basement metamorphic complex was exhumed on the earth's surface in the Middle and Late Jurassic, and extensive intermediate and acid intrusive rocks were developed in the southern North Huaiyang or northern Dabie Mountains during the basin's synde


Thrusting and Exhumation Processes of a Bounding Mountain Belt: Constraints from Sediment Provenance Analysis of the Hefei Basin
LIU Shaofeng,LIU Wencan,Faculty of Geosciences and Resources,China University of Geosciences,Beijing DAI Shaowu. Thrusting and Exhumation Processes of a Bounding Mountain Belt: Constraints from Sediment Provenance Analysis of the Hefei Basin[J]. Acta Geologica Sinica (English Edition), 2001, 75(2): 144-150. DOI: 10.1111/j.1755-6724.2001.tb00516.x
Authors:LIU Shaofeng  LIU Wencan  Faculty of Geosciences  Resources  China University of Geosciences  Beijing DAI Shaowu
Affiliation:LIU Shaofeng,LIU Wencan,Faculty of Geosciences and Resources,China University of Geosciences,Beijing DAI Shaowu,Institute of Exploration and Development,Jianghan Petroleum Administration,Guanghu,Hubei ProvinceHUANG Siji China University of Geosciences,Wuhan and LU Wuyun Anhui Bureau of Geology and Mineral Resources,Hefei
Abstract:Lithic (or gravel) composition analyses of the Jurassic Sanjianpu Formation and Fenghuangtai Formation in the Hefei basin show that the sediment provenance consists mainly of four kinds of rock units: the basement metamorphic complex, granitic rocks, medium- and low-grade metamorphic rocks, and sandy and muddy sedimentary rocks, which are distributed along the bounding thrust belt. The whole stratigrapnic section can be divided into 2 lithic sequences and 7 subsequences. The regular distribution and changes of lithic fragments and gravels in lithic (or gravel) sequences reflect that the bounding thrust belt of basin has undergone 2 thrusting cycles and 7 thrusting events. Lithic (or gravel) composition analyses of the basin fully reveal that the northern Dabie basement metamorphic complex was exhumed on the earth's surface in the Middle and Late Jurassic, and extensive intermediate and acid intrusive rocks were developed in the southern North Huaiyang or northern Dabie Mountains during the basin's syndepositional stage.
Keywords:northern Dabie Mountains   Hefei basin   sediment provenance   thrusting and exhumation
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