Mechanisms of Crustal Anatexis: a Geochemical Study of Partially Melted Metapelitic Enclaves and Host Dacite, SE Spain-Reference-Cited by-同舟云学术

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Mechanisms of Crustal Anatexis: a Geochemical Study of Partially Melted Metapelitic Enclaves and Host Dacite, SE Spain

Published:2010-02-06 Issue:4 Volume:51 Page:785-821
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:Journal of Petrology

Author:

Acosta-Vigil A.,Buick I.,Hermann J.,Cesare B.,Rubatto D.,London D.,Morgan G. B.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/51/4/785/4296868/egp095.pdf

Reference80 articles.

1. 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

2. Experiments on the kinetics of partial melting of a leucogranite at 200 MPa H2O and 690–800°C: compositional variability of melts during the onset of H2O-saturated crustal anatexis

3. Formation of elliptical garnet in a metapelitic enclave by melt-assisted dissolution and reprecipitation

4. Formation of spinel-cordierite-feldspar-glass coronas after garnet in metapelitic xenoliths: reaction modelling and geodynamic implications

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