The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: Implications for deeply subducted sediments-Reference-Cited by-同舟云学术

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The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: Implications for deeply subducted sediments

Published:1996-11 Issue:21 Volume:60 Page:4133-4150
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Domanik Kenneth J.,Holloway John R.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference63 articles.

1. B‐Be systematics in subduction-related metamorphic rocks: Characterization of the subducted component;Bebout;Geochim. Cosmochim. Acta,1993

2. Mineralogy of the Martian interior up to core-mantle boundary pressures;Bertka;J. Geophys. Res,1996

3. Vector representation of phyllosilicate compositions;Burt;Rev. Mineral.,1988

4. Magma type and crustal structure in the Aleutian arc;Coats;Geophys. Monogr.,1962

5. High-pressure structural study of muscovite;Comodi;Phys. Chem. Min.,1995

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