HIGH-PRESSURE HIGH-TEMPERATURE EVOLUTION OF FLUID INCLUSIONS IN SYNTHETIC QUARTZ

被引：54

作者：

PECHER, A ^{[1
]}

BOULLIER, AM ^{[1
]}

机构：

[1] CTR RECH PETROG & GEOCHIN,F-54501 VANDOEUVRE NANCY,FRANCE

来源：

BULLETIN DE MINERALOGIE | 1984年 / 107卷 / 02期

关键词：

D O I：

10.3406/bulmi.1984.7745

中图分类号：

P57 [矿物学];

学科分类号：

070901 ;

摘要：

引用

页码：139 / 153

页数：15

共 15 条

[1]

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[2]

BURNHAM CW, 1969, 132 GEOL SOC AM SP P

[3]

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[4]

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[5]

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[6] CONTRIBUTION TO THE EVALUATION OF INTERNAL-PRESSURE IN FLUID INCLUSIONS WHEN THEY DECREPITATE [J].

LEROY, J .

BULLETIN DE MINERALOGIE, 1979, 102 (5-6) :584-593

[7] THE MECHANISMS OF THE FORMATION AND GROWTH OF WATER BUBBLES AND ASSOCIATED DISLOCATION LOOPS IN SYNTHETIC QUARTZ [J].

MCLAREN, AC ;

COOK, RF ;

HYDE, ST ;

TOBIN, RC .

PHYSICS AND CHEMISTRY OF MINERALS, 1983, 9 (02) :79-94

[8] ROLE OF WATER IN QUARTZ DEFORMATION [J].

PATERSON, MS ;

KEKULAWALA, KRSS .

BULLETIN DE MINERALOGIE, 1979, 102 (2-3) :92-&

[9] EXPERIMENTAL DECREPITATION AND REEQUILIBRATION OF FLUID INCLUSIONS IN SYNTHETIC QUARTZ [J].

PECHER, A .

TECTONOPHYSICS, 1981, 78 (1-4) :567-583

[10]

PICHAVANT M, 1979, THESIS NANCY

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