中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Structural, metamorphic and geochronological insights on the Variscan evolution of the Alpine basement in the Belledonne Massif (France)

文献类型:期刊论文

作者Freville, Kevin1,3; Trap, Pierre2; Faure, Michel1; Melleton, Jeremie3; Li, Xian-Hua4; Lin, Wei4; Blein, Olivier3; Bruguier, Olivier5; Poujol, Marc6
刊名TECTONOPHYSICS
出版日期2018-02-15
卷号726页码:14-42
关键词Variscan Belt Alpine External Crystalline Massifs Belledonne Massif SIMS and LA-ICP-MS dating Thermobarometry Zircon and monazite dating
ISSN号0040-1951
DOI10.1016/j.tecto.2018.01.017
文献子类Article
英文摘要A structural and petrochronological study was carried out in the southern part of the Belledonne crystalline massif. A first tectonometamorphic event, Dx, corresponds to the eastward thrusting of the Chamrousse ophiolitic complex characterized by a low-temperature-moderate-pressure metamorphism reaching 0.535 +/- 0.045 GPa and 427.5 +/- 17.5 degrees C. A subsequent D-1 deformation is defined by a penetrative S-1 foliation that mostly dips toward the west and displays an E-W- to NE-SW-trending mineral and stretching lineation L-1. D-1 is associated with a top-to-the east shearing and is responsible for the crustal thickening accommodated by the eastward nappe stacking and the emplacement of the Chamrousse ophiolitic complex upon the Riouperoux-Livet unit. This event is characterized by an amphibolite facies metamorphism (0.58 GPa +/- 0.06; 608 +/- 14 degrees C) that attains partial melting at the base of the nappe pile (0.78 +/- 0.07 GPa; 680.5 +/- 11.5 degrees C). LA-ICP-MS U-Pb dating of monazite grains from the mica schists of the Riouperoux-Livet unit constrain the age of D-1 to 337 +/- 7 Ma. The D-2 tectono-metamorphic event is characterized by NE SW trending, upright to NE-verging synfolial folding. Folding associated with D-2 is pervasively developed in all lithotectonic units with the development of a steeply-dipping S-2 foliation. In particular, D-2 involves the uppermost weakly metamorphosed Taillefer unit. LA-ICP-MS U-Pb dating performed on detrital zircon grains shows that the Taillefer conglomerates was deposited during the Visean. A zircon SIMS U-Pb age of 352 +/- 1 Ma from a plagioglase-rich leucocratic sill of the Riouperoux-Livet unit is interpreted as the age of magmatic emplacement. Our results suggest that the D-2 event took place between 330 Ma and 310 Ma. We propose a new interpretation of the tectonometamorphic evolution of the southern part of the Belledonne massif, focusing on the Middle Carboniferous stages of the Variscan orogeny.
WOS关键词EXTERNAL CRYSTALLINE MASSIFS ; CHAMROUSSE OPHIOLITE COMPLEX ; FRENCH WESTERN ALPS ; TECTONIC EVOLUTION ; MIXING PROPERTIES ; U-PB ; PALEOZOIC EVOLUTION ; ARGENTERA MASSIF ; HERCYNIAN BELT ; SUTURE ZONES
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000428493800002
出版者ELSEVIER SCIENCE BV
资助机构ISTO ; ISTO ; BRGM ; BRGM ; Laboratoire Chrono-Environnement ; Laboratoire Chrono-Environnement ; Observatoire des Sciences de l'Univers en Region Centre ; Observatoire des Sciences de l'Univers en Region Centre ; ISTO ; ISTO ; BRGM ; BRGM ; Laboratoire Chrono-Environnement ; Laboratoire Chrono-Environnement ; Observatoire des Sciences de l'Univers en Region Centre ; Observatoire des Sciences de l'Univers en Region Centre ; ISTO ; ISTO ; BRGM ; BRGM ; Laboratoire Chrono-Environnement ; Laboratoire Chrono-Environnement ; Observatoire des Sciences de l'Univers en Region Centre ; Observatoire des Sciences de l'Univers en Region Centre ; ISTO ; ISTO ; BRGM ; BRGM ; Laboratoire Chrono-Environnement ; Laboratoire Chrono-Environnement ; Observatoire des Sciences de l'Univers en Region Centre ; Observatoire des Sciences de l'Univers en Region Centre
源URL[http://ir.iggcas.ac.cn/handle/132A11/83160]  
专题中国科学院地质与地球物理研究所
通讯作者Freville, Kevin
作者单位1.Univ Orleans, CNRS, Inst Sci Terre Orleans, UMR 7327, F-45071 Orleans 2, France
2.Univ Franche Comte, UMR Chronoenvironm 6249, 16 Route Gray, F-25030 Besancon, France
3.Bur Rech Geol & Minieres, Georesources Div, Mineral Deposit Studies & Dev Unit, 3 Ave Claude Guillemin,BP 36009-45060, Orleans 2, France
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
5.Univ Montpellier 2, Geosci Montpellier, Pl Eugene Bataillon, F-34095 Montpellier 5, France
6.Univ Rennes 1, OSUR, UMR CNRS 6118, Geosci Rennes, F-35042 Rennes, France
推荐引用方式
GB/T 7714
Freville, Kevin,Trap, Pierre,Faure, Michel,et al. Structural, metamorphic and geochronological insights on the Variscan evolution of the Alpine basement in the Belledonne Massif (France)[J]. TECTONOPHYSICS,2018,726:14-42.
APA Freville, Kevin.,Trap, Pierre.,Faure, Michel.,Melleton, Jeremie.,Li, Xian-Hua.,...&Poujol, Marc.(2018).Structural, metamorphic and geochronological insights on the Variscan evolution of the Alpine basement in the Belledonne Massif (France).TECTONOPHYSICS,726,14-42.
MLA Freville, Kevin,et al."Structural, metamorphic and geochronological insights on the Variscan evolution of the Alpine basement in the Belledonne Massif (France)".TECTONOPHYSICS 726(2018):14-42.

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来源:地质与地球物理研究所

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