The pressure and temperature stability limits of lawsonite: implications for H2O recycling in subduction zones-Reference-Cited by-同舟云学术

The pressure and temperature stability limits of lawsonite: implications for H2O recycling in subduction zones

Published:1994 Issue:1 Volume:118 Page:99-108
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Pawley Alison R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00310614.pdf

Reference39 articles.

1. Baur WH (1978) Crystal structure refinement of lawsonite. Am Mineral 63:311?315

2. Berman RG (1988) Internally consistent thermodynamic data for minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2. J Petrol 29:445?522

3. Berman RG (1990) Mixing properties of Ca-Mg-Fe-Mn garnets. Am Mineral 75:328?344

4. Berman RG, Brown TH, Greenwood HJ (1985) An internally consistent thermodynamic data base for minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2. Atomic Energy of Canada Ltd Technical Report 377

5. Bohlen SR, Boettcher AL (1982) The quartz-coesite transformation: a precise determination and the effects of other components. J Geophys Res 87:7073?7078

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