Equilibrium properties of granite pegmatite magmas.

C. W. Burnham; H. Nekvasil

Equilibrium properties of granite pegmatite magmas.

C. W. Burnham
, H. Nekvasil

Geosciences

Pennsylvania State University

Research output: Contribution to journal › Article › peer-review

180 Scopus citations

Abstract

A revised quasi-crystalline speciation model that incorporates a refinement of the cryoscopic equations for the major felsic melt components NaAlSi₂O₈, CaAl₂Si₂O₈, KAlSi₃O₈, and Si₄O₈ has been applied to the investigation of melt speciation behaviour in the systems: Ab-Or-Q-Sil(sillimanite)-H₂O, Ab-Q-Eu (eucryptite)-H₂O, and Ab-An-Or-Q-C(corundum)-Sp(spodumene)-H₂O-F-B. -J.A.Z.

Original language	English
Pages (from-to)	239-263
Number of pages	25
Journal	American Mineralogist
Volume	71
Issue number	3-4
State	Published - 1986

Cite this

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title = "Equilibrium properties of granite pegmatite magmas.",

abstract = "A revised quasi-crystalline speciation model that incorporates a refinement of the cryoscopic equations for the major felsic melt components NaAlSi2O8, CaAl2Si2O8, KAlSi3O8, and Si4O8 has been applied to the investigation of melt speciation behaviour in the systems: Ab-Or-Q-Sil(sillimanite)-H2O, Ab-Q-Eu (eucryptite)-H2O, and Ab-An-Or-Q-C(corundum)-Sp(spodumene)-H2O-F-B. -J.A.Z.",

author = "Burnham, \{C. W.\} and H. Nekvasil",

year = "1986",

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journal = "American Mineralogist",

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T1 - Equilibrium properties of granite pegmatite magmas.

AU - Burnham, C. W.

AU - Nekvasil, H.

PY - 1986

Y1 - 1986

N2 - A revised quasi-crystalline speciation model that incorporates a refinement of the cryoscopic equations for the major felsic melt components NaAlSi2O8, CaAl2Si2O8, KAlSi3O8, and Si4O8 has been applied to the investigation of melt speciation behaviour in the systems: Ab-Or-Q-Sil(sillimanite)-H2O, Ab-Q-Eu (eucryptite)-H2O, and Ab-An-Or-Q-C(corundum)-Sp(spodumene)-H2O-F-B. -J.A.Z.

AB - A revised quasi-crystalline speciation model that incorporates a refinement of the cryoscopic equations for the major felsic melt components NaAlSi2O8, CaAl2Si2O8, KAlSi3O8, and Si4O8 has been applied to the investigation of melt speciation behaviour in the systems: Ab-Or-Q-Sil(sillimanite)-H2O, Ab-Q-Eu (eucryptite)-H2O, and Ab-An-Or-Q-C(corundum)-Sp(spodumene)-H2O-F-B. -J.A.Z.

UR - https://www.scopus.com/pages/publications/0022858742

M3 - Article

AN - SCOPUS:0022858742

SN - 0003-004X

VL - 71

SP - 239

EP - 263

JO - American Mineralogist

JF - American Mineralogist

IS - 3-4

ER -

Equilibrium properties of granite pegmatite magmas.

Abstract

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