ROLE OF H2O IN SILICATE MELTS .2. THERMODYNAMIC AND PHASE RELATIONS IN SYSTEM NAALSI3O8-H2O TO 10 KILOBARS, 700 DEGREES CENTIGRADE TO 1100 DEGREES CENTIGRADE

被引：218

作者：

BURNHAM, CW ^{[1
]}

DAVIS, NF ^{[1
]}

机构：

[1] PENN STATE UNIV,COLL EARTH & MINERAL SCI,DEPT GEOSCI,UNIVERSITY PK,PA 16802

来源：

AMERICAN JOURNAL OF SCIENCE | 1974年 / 274卷 / 08期

关键词：

D O I：

10.2475/ajs.274.8.902

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：902 / 940

页数：39

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[3] EFFECT OF PRESSURE ON MELTING OF DIOPSIDE, CAMGSI2O6, AND ALBITE, NAALSI3O8, IN RANGE UP TO 50 KILOBARS [J].

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[6] ROLE OF H2O IN SILICATE MELTS .1. P-V-T RELATIONS IN SYSTEM NAALSI3O8-H2O TO 10 KILOBARS AND 1000 DEGREES C [J].

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[7]

BURNHAM CW, 1969, 132 GEOL SOC AM SPEC

[8]

Burnham CW, 1967, GEOCHEMISTRY HYDROTH, V20, P34

[9]

Clark S. P, 1966, HDB PHYS CONSTANTS, P415

[10]

DAVIS NF, 1972, THESIS PENNSYLVANIA

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