DIRECT DETERMINATION OF QUARTZ-COESITE TRANSITION BY INSITU X-RAY MEASUREMENTS

被引：12

作者：

BOHLER, R ^{[1
]}

ARNDT, J ^{[1
]}

机构：

[1] UNIV TUBINGEN,MINERAL PETROG INST,WILHELM STR 56,D-74 TUBINGEN,FED REP GER

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1974年 / 48卷 / 02期

关键词：

D O I：

10.1007/BF00418617

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：149 / 152

页数：4

共 14 条

[1]

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[4]

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[8] THERMODYNAMICS OF POLYMORPHIC TRANSFORMATIONS IN SILICA . THERMAL PROPERTIES FROM 5 TO 1070DEGREESK AND PRESSURE - TEMPERATURE STABILITY FIELDS FOR COESITE AND STISHOVITE [J].

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KLEPPA, OJ ;

WESTRUM, EF .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1967, 31 (12) :2289-&

[9] QUARTZ-COESITE TRANSITION [J].

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JOURNAL OF GEOPHYSICAL RESEARCH, 1964, 69 (24) :5395-+

[10] QUARTZ-COESITE STABILITY RELATIONS AT HIGH TEMPERATURES AND PRESSURES [J].

MACDONALD, GJF .

AMERICAN JOURNAL OF SCIENCE, 1956, 254 (12) :713-721

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