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
Detrital zircon age patterns from turbidites of the Balagne and Piedmont nappes of Alpine Corsica (France): Evidence for an European margin source

文献类型：期刊论文

作者Lin, Wei1,4; Rossi, Philippe2; Faure, Michel3; Li, Xian-Hua1,4; Ji, Wenbin1,4; Chu, Yang1,4
刊名TECTONOPHYSICS
出版日期2018-01-02
卷号722页码:69-105
关键词Detrital zircon provenance analysis Balagne and Piedmont nappes Alpine Corsica Piedmont-Ligurian Ocean European Tethyan Jurassic hyper-extended margin
ISSN号0040-1951
DOI10.1016/j.tecto.2017.09.015
文献子类Article
英文摘要At the front of metamorphic Cenozoic Alpine nappe of Schistes Lustres, Western Alpine Corsica (France) exposes non- to very low grade metamorphic nappes, such as the Piedmont nappes, Upper nappes, and the Balagne nappe. The provenance of the Balagne nappe remains still opened: an origin close to the Corsican continental margin; or an origin far East from the Corsican margin toward the "Apenninic" oceanic domain. This would constrain that the Balagne ophiolite be derived from the opposite OCT (Ocean - Continent transition), close to a microcontinent located to the East of the Mesozoic Corsican margin. A systematic U-Pb dating of 586 detrital zircon grains collected from the turbidites in the Balagne and Piedmont nappes has been performed to constrain the source of sediments. The zircon grains yield U-Pb age spectra ranging from Neoarchean to Late Paleozoic with age peaks at 2600 Ma, 2080 Ma, 1830 Ma, 910 Ma, 600 Ma, 560 Ma, 450 Ma, 330 Ma and 280 Ma with different continental model ages (T-DM2) from 3.5 Ga to 1.0 Ga. The variety of composition of the Corsican batholith, unique in its present Mediterranean environment, and in spite of Alpine transcurrent movements, provide a key to analyze the detrital zircon age distribution patterns of sedimentary rocks. These new results i) confirm the lack of any Cretaceous zircon that validates absence of a magmatic arc of this age, at least in the surroundings of the turbiditic formations from the Balagne and the Piedmont nappes; ii) fully support an European provenance of detritus of the Balagne nappe, iii) put forward evidence that no ophiolitic zircon was contained neither in the Cretaceous nor in the Eocene turbidites samples, and iv) question both the deposition of the Piedmont Narbinco flysch within the ocean continent transition and its possible relationships with the Late Cretaceous Pyrenean basins.
WOS关键词U-PB GEOCHRONOLOGY ; WESTERN MEDITERRANEAN REGION ; A-TYPE GRANITES ; NORTHERN CORSICA ; TRACE-ELEMENT ; ICP-MS ; CONTINENTAL-MARGIN ; LOWER-CRUST ; HERCYNIAN GRANITOIDS ; VARISCAN BATHOLITH
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000426022800006
出版者ELSEVIER SCIENCE BV
资助机构DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 41502215 ; 41502215 ; 41502215 ; 41502215 ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 41502215 ; 41502215 ; 41502215 ; 41502215 ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 41502215 ; 41502215 ; 41502215 ; 41502215 ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; DREAM project of MOST China(2016YFC0600401 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 2016YFC0600102) ; 41502215 ; 41502215 ; 41502215 ; 41502215 ; 41472193) ; 41472193) ; 41472193) ; 41472193)
源URL[http://ir.iggcas.ac.cn/handle/132A11/82882]  
专题中国科学院地质与地球物理研究所
通讯作者Lin, Wei
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.CCGM CGMW, 77 Rue Claude Bernard, F-75005 Paris, France
3.Univ Orleans, ISTO, UMR 7327, F-45071 Orleans 2, France
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714		 Lin, Wei,Rossi, Philippe,Faure, Michel,et al. Detrital zircon age patterns from turbidites of the Balagne and Piedmont nappes of Alpine Corsica (France): Evidence for an European margin source[J]. TECTONOPHYSICS,2018,722:69-105.
APA Lin, Wei,Rossi, Philippe,Faure, Michel,Li, Xian-Hua,Ji, Wenbin,&Chu, Yang.(2018).Detrital zircon age patterns from turbidites of the Balagne and Piedmont nappes of Alpine Corsica (France): Evidence for an European margin source.TECTONOPHYSICS,722,69-105.
MLA Lin, Wei,et al."Detrital zircon age patterns from turbidites of the Balagne and Piedmont nappes of Alpine Corsica (France): Evidence for an European margin source".TECTONOPHYSICS 722(2018):69-105.

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。