The H2O content of basalt glasses from Southwest Pacific back-arc basins-Reference-Cited by-同舟云学术

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The H2O content of basalt glasses from Southwest Pacific back-arc basins

Published:1993-06 Issue:3-4 Volume:117 Page:347-362
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Danyushevsky L.V.,Falloon T.J.,Sobolev A.V.,Crawford A.J.,Carroll M.,Price R.C.

Publisher

Elsevier BV

Subject

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

Reference55 articles.

1. Mariana Trough lavas from 18°N: implications for the origin of back arc basin basalts;Sinton;J. Geophys. Res.,1987

2. Volatiles in submarine glasses as a discriminant of tectonic origin: application to the Troodos ophiolite;Muenow;Nature,1990

3. Petrology and geochemistry of back-arc basin basalts from Lau Basin spreading ridges at 15, 18 and 19°S;Falloon;Mineral. Petrol.,1992

4. Mariana Trough basalts (MTB): trace element and SrNd isotopic evidence for mixing between MORB-like and arc-like melts;Volpe;Earth Planet. Sci. Lett.,1987

5. Volcanism in the Sumisu Rift, I. Major element, volatile, and stable isotope geochemistry;Hochstaedter;Earth Planet. Sci. Lett.,1990

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