KYANITE-ANDALUSITE EQUILIBRIUM

被引：30

作者：

BROWN, GC

FYFE, WS

机构：

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1971年 / 33卷 / 03期

关键词：

D O I：

10.1007/BF00374065

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：227 / &

共 10 条

[1] EXPERIMENTAL EVIDENCE THAT REACTION OF KYANITETO FORM SILLIMANITE IS AT LEAST BIVARIANT [J].

ALTHAUS, E .

AMERICAN JOURNAL OF SCIENCE, 1969, 267 (03) :273-&

[2]

Fyfe W.S., 1967, CHEM GEOL, V2, P67, DOI 10.1016/0009-2541(67)90005-8

[3] A COMBINED GRAVIMETRIC AND PHOTOMETRIC PROCEDURE FOR DETERMINING SILICA IN SILICATE ROCKS AND MINERALS [J].

JEFFERY, PG ;

WILSON, AD .

ANALYST, 1960, 85 (1012) :478-486

[4]

METZ P, 1969, DTSCH MINERAL GES BE, P32

[5] KYANITE-SILLIMANITE EQUILIBRIUM AT 750 DEGREES C [J].

NEWTON, RC .

SCIENCE, 1966, 151 (3715) :1222-&

[6] KYANITE-ANDALUSITE EQUILIBRIUM FROM 700 DEGREES TO 800 DEGREES C [J].

NEWTON, RC .

SCIENCE, 1966, 153 (3732) :170-&

[7] EXPERIMENTAL DETERMINATION OF KYANITE-ANDALUSITE AND ANDALUSITE-SILLIMANITE EQUILIBRIA - ALUMINUM SILICATE TRIPLE POINT [J].

RICHARDS.SW ;

GILBERT, MC ;

BELL, PM .

AMERICAN JOURNAL OF SCIENCE, 1969, 267 (03) :259-&

[8] THE SOLUBILITY OF QUARTZ IN H2O IN THE RANGE 1000-4000 BARS AND 400-550-DEGREES-C [J].

WEILL, DF ;

FYFE, WS .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1964, 28 (AUG) :1243-1255

[9] STABILITY RELATIONS IN AL2O3-SIO2 SYSTEM CALCULATED FROM SOLUBILITIES IN AL2O3-SIA2-NA3AIF6 SYSTEM [J].

WEILL, DF .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1966, 30 (02) :223-&

[10]

WINKLER HGF, 1970, NEUES JAHRBUCH MINER, V5, P189

← 1 →