Mechanisms of formation of barium-rich phlogopite and strontium-rich apatite during the final stages of alkaline magma evolution

Geochemistry International

Volumn 47, Issue 6, 2009, Pages 578-591

  Solovova, I P ^a   Girnis, A V ^a   Ryabchikov, I D ^a   Kononkova, N N ^b  

^a INSTITUTE OF GEOLOGY OF ORE DEPOSITS   (Russian Federation)

^b VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

BACKSCATTERED ELECTRONS; CARBONATITE; CLINOPYROXENE; COLORLESS CRYSTALS; DECOMPOSITION REACTION; DIFFERENT MECHANISMS; ENDMEMBERS; FLUID INCLUSION; FLUORAPATITE; HYDROTHERMAL SYSTEM; MAGMA EVOLUTION; MECHANISM OF FORMATION; MECHANISMS OF FORMATION; MELT-SOLUTIONS; MOBILE ELEMENTS; MOLE FRACTION; PARTITION COEFFICIENT; RARE METALS;

APATITE; BARIUM; CALCITE; CARBONATE MINERALS; CERIUM; CERIUM COMPOUNDS; CRYSTALS; ELECTRON OPTICS; FELDSPAR; FLUIDS; MICA; MINERALOGY; MINERALS; MINING; PHOSPHATE MINERALS; POTASSIUM; SILICATE MINERALS; SMELTING; STRONTIUM; TRACE ELEMENTS;

BARIUM COMPOUNDS;

APATITE; CARBONATITE; CHEMICAL COMPOSITION; CLINOPYROXENE; DECOMPOSITION; EXPERIMENTAL STUDY; FLUID INCLUSION; HYDROTHERMAL SYSTEM; MINERALIZATION; PARTITION COEFFICIENT; PHENOCRYST; PHLOGOPITE; VEIN (GEOLOGY);

EID: 67649467496     PISSN: 00167029     EISSN: None     Source Type: Journal    
DOI: 10.1134/S0016702909060044     Document Type: Article

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