DOI: 10.1007/s00531-014-1031-8
Scopus记录号: 2-s2.0-84906324670
论文题名: Variscan orogeny in Corsica: New structural and geochronological insights, and its place in the Variscan geodynamic framework
作者: Faure M. ; Rossi P. ; Gaché J. ; Melleton J. ; Frei D. ; Li X. ; Lin W.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2014
卷: 103, 期: 6 起始页码: 1533
结束页码: 1551
语种: 英语
英文关键词: Armorica
; Corsica
; Crustal melting
; Microcontinent collision
; Mid-German Crystalline Rise
; Synmetamorphic deformation
; U-Th-Pb chemical dating
; Variscan orogeny
Scopus关键词: amphibolite facies
; batholith
; Carboniferous
; crustal thickening
; ductile deformation
; geochronology
; Hercynian orogeny
; lithology
; Permian
; pluton
; structural geology
; uranium-lead dating
; Corse
; France
英文摘要: In Western Corsica, remnants of pre-batholitic lithological and metamorphic assemblages are preserved as km-scale septa enclosed within Lower Carboniferous to Early Permian plutons. Two groups of septa were recognized: (1) the Argentella and Agriates-Tenda fragments correspond to Neoproterozoic rocks deformed and metamorphosed during the Cadomian-Panafrican orogeny, and (2) the Zicavo, Porto-Vecchio, Solenzara-Fautea, Belgodère, Topiti, and Vignola fragments consist of Variscan metamorphic rocks. The lithological content and the main ductile deformation events for each septum are presented. In the Zicavo, Porto-Vecchio, and Topiti septa, a top-to-the-SW ductile shearing (D1 event) coeval with an amphibolite facies metamorphism is responsible for crustal thickening at ca 360 Ma. This main event was preceded by eclogite and granulite facies metamorphic events preserved as restites within migmatites dated at ca 345-330 Ma. A top-to-the-SE ductile shearing (D2 event) coeval with the crustal melting accommodated the exhumation of the D1 event. In contrast, the Belgodère segment is peculiar as it exhibits a top-to-the-E vergence, although retrogressed high-pressure rocks are also recognized. The pre-Permian fragments are arranged in four NW-SE-striking stripes that define a SW-NE zoning with (1) a Western domain in Topiti, Vignola, Zicavo, Porto-Vecchio, and Solenzara-Fautea; (2) a Neoproterozoic basement with its unconformable Early Paleozoic sedimentary cover in Argentella; (3) an Eastern metamorphic domain in Belgodère; (4) another Neoproterozoic basement with its Upper Paleozoic sedimentary cover in Agriates-Tenda. The Argentella basement is separated from the Western and Eastern domains by two sutures: S1 and S2. The Variscan Corsica represents the Eastern part of the Sardinia-Corsica-Maures segment. The comparison of this segment with other Variscan domains allows us to propose some possible correlations. We argue that the Western domain, Argentella, Belgodère, and Agriates-Tenda domains can be compared with the Southern Variscan belt exposed in French Massif Central-Southern Massif Armoricain, Armorica microblock, Léon block, respectively. © 2014 Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84906324670&doi=10.1007%2fs00531-014-1031-8&partnerID=40&md5=bd056903c214f965110abfd878946dc2
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70452
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
There are no files associated with this item.
作者单位: Institut des Sciences de la Terre d'Orléans, UMR CNRS 7327, Université d'Orléans, 1A rue de la Férollerie, 45067 Orléans Cedex 2, France; BRGM, Av. Claude-Guillemin, BP 36009, 45060 Orléans Cedex 2, France; U Mercatu, Lama, 20218 Ponte Leccia, France; Department of Earth Sciences, Stellenbosch University, Private Bag X1, Matieland, 7602, South Africa; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Faure M.,Rossi P.,Gaché J.,et al. Variscan orogeny in Corsica: New structural and geochronological insights, and its place in the Variscan geodynamic framework[J]. International Journal of Earth Sciences,2014-01-01,103(6)