Experimental study of the system diopside–nepheline–sanidine at 0.1, 1 and 2 GPa [P(H2O)=P(Total)]: Its significance in the genesis of alkali-rich basic and ultrabasic rocks-Reference-Cited by-同舟云学术

Experimental study of the system diopside–nepheline–sanidine at 0.1, 1 and 2 GPa [P(H2O)=P(Total)]: Its significance in the genesis of alkali-rich basic and ultrabasic rocks

Published:2006-01 Issue:1-2 Volume:86 Page:91-109
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Gupta Alok K.,Chattopadhyay S.,Chattopadhyay B.,Arima Makoto

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference48 articles.

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4. Phase relationships in the system NaAlSiO4–SiO2–H2O at 35 kbar pressure;Boettcher;Am. J. Sci.,1969

5. Reinvestigation and application of olivine–quartz–orthopyroxene-boundary;Bohlen;Earth Planet. Sci. Lett.,1980

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