Temporal control of subduction magmatism in the eastern Trans-Mexican Volcanic Belt: Mantle sources, slab contributions, and crustal contamination-Reference-Cited by-同舟云学术

Temporal control of subduction magmatism in the eastern Trans-Mexican Volcanic Belt: Mantle sources, slab contributions, and crustal contamination

Published:2003-08 Issue:8 Volume:4 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Gómez-Tuena Arturo¹,LaGatta Alexandra B.²,Langmuir Charles H.³,Goldstein Steven L.²,Ortega-Gutiérrez Fernando⁴,Carrasco-Núñez Gerardo¹

Affiliation:

1. Centro de Geociencias; Universidad Nacional Autónoma de México; Campus Juriquilla, Querétaro 76230 México

2. Lamont Doherty Earth Observatory of Columbia University; Palisades New York 10960 USA

3. Department of Earth and Planetary Sciences; Harvard University; Cambridge Massachusetts 02138 USA

4. Instituto de Geología; Universidad Nacional Autónoma de México; Ciudad Universitaria, Coyoacán 04510 México City México

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference99 articles.

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3. Partial melting in Archean subduction zones: Constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions;Barth;Precambrian Res.,2002

4. Geochemical constraints on the origin of the calc-alkaline and alkaline magmas of the eastern Trans-Mexican Volcanic Belt;Besch;Geofis. Int.,1988

5. The variable role of slab derived fluids in the generation of a suite of primitive calc-alkaline lavas from the southernmost Cascades, California;Borg;Can. Mineral.,1997

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