THERMODYNAMIC STUDY OF PSEUDOBINARY JOIN MUSCOVITE-PARAGONITE IN SYSTEM KALSI3O8-NAALSI3O8-AL2O3-SIO2-H2O

被引：0

作者：

CHATTERJEE, ND

FROESE, E

机构：

[1] RUHR UNIV,INST MINERAL,4630 BOCHUM,FED REP GER

[2] GEOL SURVEY CANADA,601 BOOTH ST,OTTAWA,ONTARIO,CANADA

来源：

AMERICAN MINERALOGIST | 1975年 / 60卷 / 11-1期

关键词：

D O I：

暂无

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：985 / 993

页数：9

共 50 条

[1] STABILITY OF PARAGONITE IN SYSTEM SIO2-NAALSI3O8-AL2O3-H2O
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[4] REACTION DECHANGE DIONS NA-K DANS LA SERIE MUSCOVITE-PARAGONITE . CONTRIBUTION A LETUDE DU SYSTEME AL2O3-NAALSI3O8-KALSI3O8-H2O
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[6] A PHASE-EQUILIBRIUM STUDY IN THE SYSTEM KALSI3O8-NAALSI3O8-SIO2-AL2SIO5-H2O AND PETROGENETIC IMPLICATIONS
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[8] SUBSOLIDUS CRYSTALLIZATION BEHAVIOUR IN SYSTEM KALSI3O8-NAALSI3O8-H2O
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[9] A thermodynamic model for hydrous silicate melts in the system NaAlSi3O8-KAlSi3O8-Si4O8-H2O
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[10] Compositional dependence of H2O solubility along the joins NaAlSi3O8-KAlSi3O8, NaAlSi3O8-LiAlSi3O8, and KAlSi3O8-LiAlSi3O8
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