中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Syn-collisional channel flow and exhumation of Paleoproterozoic high pressure rocks in the Trans-North China Orogen: The critical role of partial-melting and orogenic bending

文献类型:期刊论文

作者Trap, Pierre1; Faure, Michel2; Lin, Wei3; Augier, Romain2; Fouassier, Antoine2
刊名GONDWANA RESEARCH
出版日期2011-09-01
卷号20期号:2-3页码:498-515
关键词High-pressure rocks Exhumation Partial melting Channel flow Trans-North China Orogen
ISSN号1342-937X
DOI10.1016/j.gr.2011.02.013
文献子类Article
英文摘要Within the paleoproterozoic Trans-North China Orogen, the High-Pressure Belt (HPB) is made of high-pressure (similar to 15 kbar) mafic granulites hosted in migmatitic gneisses. In this contribution, we document a set of structural analyses acquired over the whole HPB. We also proposed a morphological subdivision of the partially molten rocks that compose the HPB according to changes in melt fraction. A compilation of the P-T and radiochronological data carried out over the last 15 years is presented. The results highlight the concurrent effect of oroclinal bending and partial-melting in controlling the exhumation of the deeply buried continental crust.
WOS关键词PB ZIRCON GEOCHRONOLOGY ; HIMALAYAN-TIBETAN OROGEN ; LOWER CRUSTAL SECTION ; U-PB ; TECTONIC EVOLUTION ; HENGSHAN COMPLEX ; COLUMBIA SUPERCONTINENT ; METAMORPHIC EVOLUTION ; DEFORMATION HISTORY ; NUMERICAL-MODELS
WOS研究方向Geology
语种英语
WOS记录号WOS:000294075700016
出版者ELSEVIER SCIENCE BV
资助机构National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116) ; National Science Foundation of China(40472116)
源URL[http://ir.iggcas.ac.cn/handle/132A11/74072]  
专题中国科学院地质与地球物理研究所
通讯作者Trap, Pierre
作者单位1.Univ Franche Comte, UMR CNRS Chronoenvironm 6249, F-25030 Besancon, France
2.Univ Orleans, CNRS, UMR 6113, Inst Sci Terre Orleans, F-45067 Orleans 2, France
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Trap, Pierre,Faure, Michel,Lin, Wei,et al. Syn-collisional channel flow and exhumation of Paleoproterozoic high pressure rocks in the Trans-North China Orogen: The critical role of partial-melting and orogenic bending[J]. GONDWANA RESEARCH,2011,20(2-3):498-515.
APA Trap, Pierre,Faure, Michel,Lin, Wei,Augier, Romain,&Fouassier, Antoine.(2011).Syn-collisional channel flow and exhumation of Paleoproterozoic high pressure rocks in the Trans-North China Orogen: The critical role of partial-melting and orogenic bending.GONDWANA RESEARCH,20(2-3),498-515.
MLA Trap, Pierre,et al."Syn-collisional channel flow and exhumation of Paleoproterozoic high pressure rocks in the Trans-North China Orogen: The critical role of partial-melting and orogenic bending".GONDWANA RESEARCH 20.2-3(2011):498-515.

入库方式: OAI收割

来源:地质与地球物理研究所

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