Oxygen isotope evidence for slab melting in modern and ancient subduction zones-Reference-Cited by-同舟云学术

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Oxygen isotope evidence for slab melting in modern and ancient subduction zones

Published:2005-07 Issue:3-4 Volume:235 Page:480-496
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bindeman I.N.,Eiler J.M.,Yogodzinski G.M.,Tatsumi Y.,Stern C.R.,Grove T.L.,Portnyagin M.,Hoernle K.,Danyushevsky L.V.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference62 articles.

1. Orogenic Andesites and Plate Tectonics;Gill,1981

2. Tracers of the slab. Inside the subduction factory;Elliot;Geophys. Monogr.,2003

3. Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas;Martin;Geology,1986

4. Aleutian magnesian andesites: melts from subducted Pacific ocean crust;Kay;J. Volcanol. Geotherm. Res.,1978

5. Role of the subducted slab, mantle wedge and continental crust in the generation of adakites from the Andean Austral volcanic zone;Stern;Contrib. Mineral. Petrol.,1996

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