The stability of sapphirine + clinopyroxene: implications for phase relations in the CaO-MgO-Al2O3-SiO2 system under deep-crustal and upper mantle conditions-Reference-Cited by-同舟云学术

The stability of sapphirine + clinopyroxene: implications for phase relations in the CaO-MgO-Al2O3-SiO2 system under deep-crustal and upper mantle conditions

Published:1989-08 Issue:4 Volume:102 Page:422-428
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Christy Andrew G.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00371085.pdf

Reference30 articles.

1. Ackermand D, Seifert F (1975) The instability of sapphirine at high pressures. Contrib Mineral Petrol 50:79?92

2. Barbier J, Hyde BG (1988) The structure of sapphirine: its relationship to the spinel, clinopyroxene and ?-gallia structures. Acta Crystallogr B44:373?376

3. Christy AG, Putnis A (1988) Planar and line defects in the sapphirine polytypes. Phys Chem Mineral (in press)

4. Cosca MA, Rouse RC, Essene EJ (1988) Dorrite, [Ca2(Mg2-Fe4/3+)(Al4Si2)O20], a new member of the aenigmatite group from a pyrometamorphic melt-rock. Am Mineral (in press)

5. Dymek RF, Gromet LP (1984) Nature and origin of orthopyroxene megacrysts from the St. Urbain massif, Quebec. Can Mineral 22:297?326

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