High-pressure and high-temperature stability of chlorite and 23-Å phase in the natural chlorite and synthetic MASH system-Reference-Cited by-同舟云学术

High-pressure and high-temperature stability of chlorite and 23-Å phase in the natural chlorite and synthetic MASH system

Published:2019-02 Issue:2-3 Volume:351 Page:104-112
ISSN:1631-0713
Container-title:Comptes Rendus Geoscience
language:en
Short-container-title:Comptes Rendus Geoscience

Author:

Cai Nao,Inoue Toru

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,Global and Planetary Change

Reference33 articles.

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2. The stability of antigorite in the systems MgO–SiO2–H2O (MSH) and MgO–Al2O3–SiO2–H2O (MASH): The effects of Al3+ substitution on high-pressure stability;Bromiley;Am. Mineral.,2003

3. A possible new Al-bearing hydrous Mg-silicate (23 angstrom phase) in the deep upper mantle;Cai;Am. Mineral.,2015

4. Phase relationships of chlorites in the system MgO–Al2O3–SiO2–H2O;Fawcett;Am. Mineral.,1966

5. New experimental results up to 100 kbar in the system MgOAl2O3-SiO2-H2O (MASH): Preliminary stability fields of chlorite, chloritoid, staurolite, MgMgAl-pumpellyite, and pyrope;Fockenberg;Bochumer Geologischeand Geotechnische Arbeiten,1995

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