中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China

文献类型：期刊论文

作者Faure, Michel1,2; Shu, Liangshu3; Wang, Bo3; Charvet, Jacques1; Choulet, Flavien1; Monie, Patrick4
刊名TERRA NOVA
出版日期2009-10-01
卷号21期号:5页码:360-368
ISSN号0954-4879
DOI10.1111/j.1365-3121.2009.00888.x
文献子类Article
英文摘要The Early Palaeozoic Orogen of SE China consists of three litho-tectonic elements, from top to bottom: a sedimentary Upper Unit, a metamorphic Lower Unit and a gneissic basement. The boundaries between these units are flat lying, south directed, ductile decollements. The lower one is coeval with an amphibolite facies metamorphism (M1). The belt is reworked by migmatite-granite domes, high-temperature metamorphism (M2) and granitic plutons related to post-orogenic crustal melting. We date here the syn-M1 ductile shearing at 453 +/- 7 Ma by U-Th/Pb method on monazite. Previous ages and our new
WOS关键词SOUTH CHINA ; U-PB ; SOUTHEASTERN CHINA ; JIANGXI PROVINCE ; CATHAYSIA BLOCK ; TECTONIC EVOLUTION ; TIEN-SHAN ; SM-ND ; AGE ; COLLISION
WOS研究方向Geology
语种英语
WOS记录号WOS:000269732400004
出版者WILEY-BLACKWELL
资助机构National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; National Natural Science Foundation of China(40634022) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; Chinese Academy of Sciences(KZCX1-YW-15-1) ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing ; State Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Academy of Sciences, Beijing
源URL[http://ir.iggcas.ac.cn/handle/132A11/71922]  
专题中国科学院地质与地球物理研究所
通讯作者Faure, Michel
作者单位1.Univ Orleans, CNRS, INSU, Univ Tours,Inst Sci Terre Orleans,UMR 6113, F-45071 Orleans 2, France
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Nanjing Univ, Dept Earth Sci, Nanjing 210008, Peoples R China
4.Univ Montpellier 2, UMR 5243, F-34095 Montpellier, France
推荐引用方式
GB/T 7714		 Faure, Michel,Shu, Liangshu,Wang, Bo,et al. Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China[J]. TERRA NOVA,2009,21(5):360-368.
APA Faure, Michel,Shu, Liangshu,Wang, Bo,Charvet, Jacques,Choulet, Flavien,&Monie, Patrick.(2009).Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China.TERRA NOVA,21(5),360-368.
MLA Faure, Michel,et al."Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China".TERRA NOVA 21.5(2009):360-368.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。