Multi-stage evolution of the lithospheric mantle beneath the westernmost Mediterranean: Geochemical constraints from peridotite xenoliths in the eastern Betic Cordillera (SE Spain)-Reference-Cited by-同舟云学术

Multi-stage evolution of the lithospheric mantle beneath the westernmost Mediterranean: Geochemical constraints from peridotite xenoliths in the eastern Betic Cordillera (SE Spain)

Published:2017-04 Issue: Volume:276 Page:75-89
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Marchesi Claudio,Konc Zoltán,Garrido Carlos J.,Bosch Delphine,Hidas Károly,Varas-Reus María Isabel,Acosta-Vigil Antonio

Funder

Spanish “Ministerio de Economía y Competitividad” (MINECO)

Università di Padova (Italy)

MINECO

Junta de Andalucía

International Lithosphere Program

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference83 articles.

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3. Crustal trace element and isotopic signatures in garnet pyroxenites from garnet peridotite massifs from Lower Austria;Becker;Journal of Petrology,1996

4. Distribution of incompatible trace elements between the constituents of spinel peridotite xenoliths: ICP-MS data from the East African Rift;Bedini;Geochimica et Cosmochimica Acta,1999

5. Mantle xenoliths from Tallante (Betic Cordillera): insights into the multi-stage evolution of the south Iberian lithosphere;Bianchini;Lithos,2011

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