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The architecture of the European-Mediterranean lithosphere: A synthesis of the Re-Os evidence

2013; Geological Society of America; Volume: 41; Issue: 5 Linguagem: Inglês

10.1130/g34003.1

1943-2682

José María González-Jiménez, Carlos Villaseca, William L. Griffin, Елена Белоусова, Zoltán Konc, Eumenio Ancochea Soto, Suzanne Y. O’Reilly, Norman J. Pearson, Carlos J. Garrido, Fernando Gervilla,

earthquake and tectonic studies

Research Article| May 01, 2013 The architecture of the European-Mediterranean lithosphere: A synthesis of the Re-Os evidence José M. González-Jiménez; José M. González-Jiménez 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Search for other works by this author on: GSW Google Scholar Carlos Villaseca; Carlos Villaseca 2Departamento de Petrología y Geoquímica, Universidad Complutense de Madrid, and Instituto de Geosciencias (UCM-CSIC), 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar William L. Griffin; William L. Griffin 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Search for other works by this author on: GSW Google Scholar Elena Belousova; Elena Belousova 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Search for other works by this author on: GSW Google Scholar Zoltan Konc; Zoltan Konc 3Instituto Andaluz de Ciencias de la Tierra (IACT), CSIC-UGR, 18100 Armilla, Granada, Spain Search for other works by this author on: GSW Google Scholar Eumenio Ancochea; Eumenio Ancochea 2Departamento de Petrología y Geoquímica, Universidad Complutense de Madrid, and Instituto de Geosciencias (UCM-CSIC), 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar Suzanne Y. O'Reilly; Suzanne Y. O'Reilly 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Search for other works by this author on: GSW Google Scholar Norman J. Pearson; Norman J. Pearson 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Search for other works by this author on: GSW Google Scholar Carlos J. Garrido; Carlos J. Garrido 3Instituto Andaluz de Ciencias de la Tierra (IACT), CSIC-UGR, 18100 Armilla, Granada, Spain Search for other works by this author on: GSW Google Scholar Fernando Gervilla Fernando Gervilla 4Departamento de Mineralogía y Petrología, Universidad de Granada, and Instituto Andaluz de Ciencias de la Tierra (IACT), UGR-CSIC, Facultad de Ciencias, 18002 Granada, Spain Search for other works by this author on: GSW Google Scholar Author and Article Information José M. González-Jiménez 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Carlos Villaseca 2Departamento de Petrología y Geoquímica, Universidad Complutense de Madrid, and Instituto de Geosciencias (UCM-CSIC), 28040 Madrid, Spain William L. Griffin 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Elena Belousova 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Zoltan Konc 3Instituto Andaluz de Ciencias de la Tierra (IACT), CSIC-UGR, 18100 Armilla, Granada, Spain Eumenio Ancochea 2Departamento de Petrología y Geoquímica, Universidad Complutense de Madrid, and Instituto de Geosciencias (UCM-CSIC), 28040 Madrid, Spain Suzanne Y. O'Reilly 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Norman J. Pearson 1ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Carlos J. Garrido 3Instituto Andaluz de Ciencias de la Tierra (IACT), CSIC-UGR, 18100 Armilla, Granada, Spain Fernando Gervilla 4Departamento de Mineralogía y Petrología, Universidad de Granada, and Instituto Andaluz de Ciencias de la Tierra (IACT), UGR-CSIC, Facultad de Ciencias, 18002 Granada, Spain Publisher: Geological Society of America Received: 30 Aug 2012 Revision Received: 18 Nov 2012 Accepted: 25 Nov 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (5): 547–550. https://doi.org/10.1130/G34003.1 Article history Received: 30 Aug 2012 Revision Received: 18 Nov 2012 Accepted: 25 Nov 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation José M. González-Jiménez, Carlos Villaseca, William L. Griffin, Elena Belousova, Zoltan Konc, Eumenio Ancochea, Suzanne Y. O'Reilly, Norman J. Pearson, Carlos J. Garrido, Fernando Gervilla; The architecture of the European-Mediterranean lithosphere: A synthesis of the Re-Os evidence. Geology 2013;; 41 (5): 547–550. doi: https://doi.org/10.1130/G34003.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Rhenium-depletion model ages (TRD) of sulfides in peridotite xenoliths from the subcontinental mantle beneath central Spain (the Calatrava volcanic field) reveal that episodes of mantle magmatism and/or metasomatism in the Iberia microplate were linked to crustal growth events, mainly during supercontinent assembly and/or breakup at ca. 1.8, 1.1, 0.9, 0.6, and 0.3 Ga. A synthesis of available in situ and whole-rock Os-isotope data on mantle-derived peridotites shows that this type of mantle (maximum TRD of ca. 1.8 Ga) is widespread in the subcontinental mantle of Europe and Africa outboard from the Betics-Maghrebides-Appenines front. In contrast, the mantle enclosed within the Alpine domain records TRD as old as 2.6 Ga, revealing a previously unrecognized Archean domain or domains in the central and western Mediterranean. Our observations indicate that ancient fragments of subcontinental lithospheric mantle have played an important role in the development of the present architecture of the Mediterranean lithosphere. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.