Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a similar to 2.1 Ga thermal and tectonic event in the Fuping Massif
文献类型：期刊论文
| 作者 | Trap, P.1; Faure, M.1; Lin, W.2; Bruguier, O.3; Monie, P.4 |
| 刊名 | JOURNAL OF STRUCTURAL GEOLOGY
 |
| 出版日期 | 2008 |
| 卷号 | 30期号:9页码:1109-1125 |
| 关键词 | Trans-North China Belt Paleoproterozoic geodynamics Dome-and-basin structure Ductile shearing Syntectonic plutonism |
| ISSN号 | 0191-8141 |
| DOI | 10.1016/j.jsg.2008.05.001 |
| 文献子类 | Article |
| 英文摘要 | Structural analysis along with (40)Ar-(39)Ar and U-Pb datings in the Fuping massif provide new insight into the evolution of the eastern part of the Trans-North China Belt (North China Craton), from 2.7 Ga to 1.8 Ga. D1 is responsible for the development of a dome-and-basin structure coeval with crustal melting giving rise to migmatite and Nanying gneissic granites at 2.1 Ga. This dome-and-basin architecture resulted from the interference between a N-S compression of a weak ductile crust and gravity-driven vertical flow, in a high thermal regime. The next events involved flat lying ductile thrusting (D2) and normal faulting (D3) dated at around 1880 Ma and 1830 Ma, respectively. The D2 and D3 events belong to the Trans-North China Orogeny that results in the final amalgamation of the North China Craton. The D1 deformation is considered as evidence for an earlier orogen developed around 2.1 Ga prior to the Trans-North China Orogeny. The change in the deformation style between the 2.1 Ga and 1.8 Ga could be viewed as a consequence of the cooling of the continental crust in the North China Craton. (C) 2008 Published by Elsevier Ltd. |
| WOS关键词 | PB ZIRCON GEOCHRONOLOGY ; ARCHEAN DHARWAR CRATON ; CENTRAL ZONE ; CONTINENTAL-CRUST ; STRAIN PATTERNS ; WUTAISHAN AREA ; GNEISS DOMES ; SOUTH-INDIA ; COMPLEX ; CONSTRAINTS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000259884000004 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 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/132A11/69464]  |
| 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 Orleans, CNRS, UMR 6113, Inst Sci Terre Orleans, F-45067 Orleans 2, France 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 3.Univ Montpellier 2, Serv Commun ICP MS, ISTEEM, F-34095 Montpellier 5, France 4.Univ Montpellier 2, CNRS, UMR 5243, F-34095 Montpellier 5, France |
| 推荐引用方式 GB/T 7714 | Trap, P.,Faure, M.,Lin, W.,et al. Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a similar to 2.1 Ga thermal and tectonic event in the Fuping Massif[J]. JOURNAL OF STRUCTURAL GEOLOGY,2008,30(9):1109-1125. |
| APA | Trap, P.,Faure, M.,Lin, W.,Bruguier, O.,&Monie, P..(2008).Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a similar to 2.1 Ga thermal and tectonic event in the Fuping Massif.JOURNAL OF STRUCTURAL GEOLOGY,30(9),1109-1125. |
| MLA | Trap, P.,et al."Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a similar to 2.1 Ga thermal and tectonic event in the Fuping Massif".JOURNAL OF STRUCTURAL GEOLOGY 30.9(2008):1109-1125. |
入库方式： OAI收割
来源：地质与地球物理研究所
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