The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen
文献类型：期刊论文
| 作者 | Trap, P.1; Faure, M.1; Lin, W.2; Monie, P.3; Meffre, S.4; Melleton, J.1,5 |
| 刊名 | PRECAMBRIAN RESEARCH
 |
| 出版日期 | 2009-07-01 |
| 卷号 | 172期号:1-2页码:80-98 |
| 关键词 | Trans-North China Orogen Structural analysis North China Craton Paleoproterozoic geodynamics Zanhuang Massif |
| ISSN号 | 0301-9268 |
| DOI | 10.1016/j.precamres.2009.03.011 |
| 文献子类 | Article |
| 英文摘要 | This paper presents a reappraisal of the tectonic evolution of the Zanhuang Massif that lies at the eastern margin of the Trans-North China Orogen, a continent-continent collision belt that marked the amalgamation of the North China Craton in Late Paleoproterozoic. Detailed field work with focus on geometries of structures and kinematics was performed. This was completed with LA-ICP-MS U-Pb analyses on zircon, EPMA U-Th/Pb dating on monazite and (40)Ar/(39)Ar dating on amphibole. These studies led us to propose a new three-fold litho-tectonic subdivision of the massif. The Western Zanhuang Domain (WZD) made of TTG, migmatite and pink anatectic granite is correlated to the Fuping Massif that crops out to the north-west. Both areas represent a continental block, called the Fuping Block, which acquired most of its architecture around 2100 Ma ago. The Eastern Zanhuang Domain (EZD) made of TTG and migmatite represents the western edge of an Eastern Neoarchean Block. In between, the Central Zanhuang Domain (CZD) is a NE-SW trending stack of supracrustal, gneiss and mafic magmatic rocks thrust sheets displaced toward the ESE upon the Eastern Block. The lithological features suggest that the CZD represents the remnant of an oceanic basin, called the Taihang Ocean that closed during the amalgamation of the Eastern Block and the Fuping Block around 1880-1850 Ma. In agreement with recent work done along the western margin of the belt, in the Luliang Massif, this study documents the amalgamation of the North China Craton in response to the closure of two oceanic basins, namely the Luliang Ocean and the Taihang Ocean. West-dipping subductions and collisions involving three distinct continental blocks, called the Western, the Fuping and the Eastern Blocks, took place around 1880-1850 Ma. (C) 2009 Elsevier B.V. All rights reserved. |
| WOS关键词 | LITHOSPHERIC MANTLE BENEATH ; HIGH-PRESSURE GRANULITES ; PB ZIRCON AGES ; U-TH-PB ; TECTONIC EVOLUTION ; METAMORPHIC EVOLUTION ; ISOTOPIC CONSTRAINTS ; CONTINENTAL-CRUST ; TAIHANG MOUNTAINS ; HENGSHAN COMPLEX |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000267148900005 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | National Science Foundation of China, NSFC(40472116 ; National Science Foundation of China, NSFC(40472116 ; 40730315) ; 40730315) ; National Science Foundation of China, NSFC(40472116 ; National Science Foundation of China, NSFC(40472116 ; 40730315) ; 40730315) ; National Science Foundation of China, NSFC(40472116 ; National Science Foundation of China, NSFC(40472116 ; 40730315) ; 40730315) ; National Science Foundation of China, NSFC(40472116 ; National Science Foundation of China, NSFC(40472116 ; 40730315) ; 40730315) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/71696]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Trap, P. |
| 作者单位 | 1.Univ Tours, Univ Orleans, CNRS, INSU,Inst Sci Terre Orleans,UMR 6113, F-45071 Orleans 2, France 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithosphere Evolut, Beijing 100029, Peoples R China 3.Univ Montpellier 2, CNRS, UMR 5243, F-34095 Montpellier 5, France 4.Univ Tasmania, ARC Ctr Excellence Ore Deposits, Hobart, Tas 7001, Australia 5.Bur Rech Geol & Minieres, F-45060 Orleans 2, France |
| 推荐引用方式 GB/T 7714 | Trap, P.,Faure, M.,Lin, W.,et al. The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen[J]. PRECAMBRIAN RESEARCH,2009,172(1-2):80-98. |
| APA | Trap, P.,Faure, M.,Lin, W.,Monie, P.,Meffre, S.,&Melleton, J..(2009).The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen.PRECAMBRIAN RESEARCH,172(1-2),80-98. |
| MLA | Trap, P.,et al."The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen".PRECAMBRIAN RESEARCH 172.1-2(2009):80-98. |
入库方式： OAI收割
来源：地质与地球物理研究所
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