中生代盆地演化及其对大别造山带碰撞造山的指示意义
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引用本文:LIU Shao-feng.2012.中生代盆地演化及其对大别造山带碰撞造山的指示意义[J].地球学报,33(s1):39.
DOI:10.3975/cagsb.2012.s1.20
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作者单位E-mail
LIU Shao-feng State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing) shaofeng@cugb.edu.cn 
中文摘要:The Dabie orogenic belt underwent deep subduc-tion of continent, rapid exhumation, and huge amount of erosion during the Mesozoic. Its tectonic evolution, especially how that was recorded in sedimentary ba-sins at the flanks of the Dabie orogenic belt is one of the most important issues. The overall distribution of different basin types in the orogenic belt indicates that shortening and thrusting at the margins of the orogenic belt from the Late Triassic to the Early Cretaceous controlled the foreland basins, and extension, doming and rifting were initiated in the core of the orogenic belt from the Jurassic to the Early Cretaceous, and were expanded to the whole orogenic belt after the Late Cretaceous.
中文关键词:Dabie orogenic belt  Collisional orogeny  Sedimentary basin  Mesozoic
 
Mesozoic Basin Development and Its Indication of Collisional Orogeny in the Dabie Orogenic Belt
Abstract:The Dabie orogenic belt underwent deep subduc-tion of continent, rapid exhumation, and huge amount of erosion during the Mesozoic. Its tectonic evolution, especially how that was recorded in sedimentary ba-sins at the flanks of the Dabie orogenic belt is one of the most important issues. The overall distribution of different basin types in the orogenic belt indicates that shortening and thrusting at the margins of the orogenic belt from the Late Triassic to the Early Cretaceous controlled the foreland basins, and extension, doming and rifting were initiated in the core of the orogenic belt from the Jurassic to the Early Cretaceous, and were expanded to the whole orogenic belt after the Late Cretaceous.
keywords:Dabie orogenic belt  Collisional orogeny  Sedimentary basin  Mesozoic
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