The evolution of magma during continental rifting: New constraints from the isotopic and trace element signatures of silicic magmas from Ethiopian volcanoes-Reference-Cited by-同舟云学术

The evolution of magma during continental rifting: New constraints from the isotopic and trace element signatures of silicic magmas from Ethiopian volcanoes

Published:2018-05 Issue: Volume:489 Page:203-218
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Hutchison William^ORCID,Mather Tamsin A.,Pyle David M.,Boyce Adrian J.,Gleeson Matthew L.M.,Yirgu Gezahegn,Blundy Jon D.,Ferguson David J.,Vye-Brown Charlotte,Millar Ian L.,Sims Kenneth W.W.,Finch Adrian A.

Funder

NERC

Horizon 2020

Publisher

Elsevier BV

Subject

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

Reference95 articles.

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3. Experimental determination of oxygen isotope fractionations between CO2 vapor and soda-melilite melt;Appora;Geochim. Cosmochim. Acta,2003

4. Upper mantle temperature and the onset of extension and break-up in Afar, Africa;Armitage;Earth Planet. Sci. Lett.,2015

5. Source, genesis, and timing of giant ignimbrite deposits associated with Ethiopian continental flood basalts;Ayalew;Geochim. Cosmochim. Acta,2002

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