The composition of nanogranitoids in migmatites overlying the Ronda peridotites (Betic Cordillera, S Spain): the anatectic history of a polymetamorphic basement-Reference-Cited by-同舟云学术

The composition of nanogranitoids in migmatites overlying the Ronda peridotites (Betic Cordillera, S Spain): the anatectic history of a polymetamorphic basement

Published:2016-02-25 Issue:3 Volume:171 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Acosta-Vigil Antonio,Barich Amel,Bartoli Omar,Garrido Carlos J.,Cesare Bernardo,Remusat Laurent,Poli Stefano,Raepsaet Caroline

Funder

European Commission, Marie Curie Actions

Ministerio de Economía y Competitividad (ES)

Consejería de Economía, Innovación, Ciencia y Empleo, Junta de Andalucía (ES)

Italian Ministry of Education, University and Research

Università degli Studi di Padova (IT)

Instituto Andaluz de Ciencias de la Tierra

European Union Cohesion Policy funds

Università degli Studi di Padova - European Commission, Marie Curie Actions

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-016-1230-3.pdf

Reference159 articles.

1. Acosta A (1998) Estudio de los fenómenos de fusión cortical y generación de granitoides asociados a las peridotitas de Ronda. Unpublished Ph.D. Thesis, Universidad de Granada, p 305

2. Acosta-Vigil A, Pereira MD, Shaw DM, London D (2001) Contrasting behaviour of B during crustal anatexis. Lithos 56:15–31

3. Acosta-Vigil A, London D, Dewers TA, Morgan GB VI (2002) Dissolution of corundum and andalusite in H2O-saturated haplogranitic melts at 800°C and 200 MPa: constraints on diffusivities and the generation of peraluminous melts. J Petrol 43:1885–1908

4. Acosta-Vigil A, London D, Morgan GB VI, Dewers TA (2003) Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700–800 °C and 200 MPa, and applications of the aluminum saturation index. Contrib Mineral Petrol 146:100–119

5. Acosta-Vigil A, London D, Morgan GB VI, Dewers TA (2006a) Dissolution of quartz, albite, and orthoclase in H2O-saturated haplogranitic melts at 800°C and 200 MPa: diffusive transport properties of granitic melts at crustal anatectic conditions. J Petrol 47:231–254

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