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• W2115087208 abstract "Research Article| July 01, 2005 Early Mesozoic thrust tectonics of the northwest Zhejiang region (Southeast China) Wenjiao Xiao; Wenjiao Xiao 1State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China Search for other works by this author on: GSW Google Scholar Haiqing He Haiqing He 2Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083, China Search for other works by this author on: GSW Google Scholar GSA Bulletin (2005) 117 (7-8): 945–961. https://doi.org/10.1130/B25417.1 Article history received: 05 Jun 2003 rev-recd: 13 Jul 2004 accepted: 03 Jan 2005 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Wenjiao Xiao, Haiqing He; Early Mesozoic thrust tectonics of the northwest Zhejiang region (Southeast China). GSA Bulletin 2005;; 117 (7-8): 945–961. doi: https://doi.org/10.1130/B25417.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The NW Zhejiang region of South China occupies a key tectonic position near the suture zone of the Yangtze and Cathaysian blocks and is of critical importance for the assembly of East Asia. Sedimentological and tectonic analyses indicate that the region had a SE-dipping paleoslope in the late Paleozoic to Early Triassic. A transitional sedimentary environment from deep sea to continental molasse is documented in the early Triassic–late Triassic interval. Associated structures are NW-vergent folds and thrusts that root southeastward beneath the high-grade Chencai metamorphic complex. The structural styles of this foreland fold-and-thrust belt are characterized by multifold duplexes and individual folds that are together zoned from SE to NW as follows: (1) core zone characterized by shear folds and ductile thrusts; (2) SE belt with out-of-sequence thrusting of multifold duplexes and an average shortening of 50%; (3) central belt with duplexes, imbricate fans, and an average shortening of 40%; and (4) NW belt with Jura-type folds and a shortening of ∼10%. A tectonic model for the foreland fold-and-thrust belt is discussed in relation to the early Mesozoic archipelago paleogeography of South China. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2115087208 date "2005-01-01" @default.
• W2115087208 modified "2023-09-30" @default.
• W2115087208 title "Early Mesozoic thrust tectonics of the northwest Zhejiang region (Southeast China)" @default.
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• W2115087208 doi "https://doi.org/10.1130/b25417.1" @default.
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