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TSCHERMAK SUBSTITUTION IN THE ASSEMBLAGE MUSCOVITE PLUS BIOTITE PLUS CHLORITE PLUS QUARTZ - A COMPARISON BETWEEN NATURAL AND THERMODYNAMIC DATA
Uppsala University.
1995 (English)In: NEUES JAHRBUCH FUR MINERALOGIE-MONATSHEFTE, ISSN 0028-3649, no 2, 75-95 p.Article in journal (Other scientific) Published
Abstract [en]

In the system K2O-FeO-MgO-Al2O3-SiO2-H2O (KFMASH) the assemblage muscovite + biotite + chlorite + quartz + water is constrained by the reactions Mg-1Si-1Al2[MUS] = Mg-1Si-1Al2[BIO] (1b) Mg-1Si-1Al2[MUS] = Mg-1Si-1Al2[CHL] (2b) Mg-1Fe[MUS] = Mg-1Fe[BIO] (3

Place, publisher, year, edition, pages
E SCHWEIZERBART'SCHE VERLAGS , 1995. no 2, 75-95 p.
Keyword [en]
TSCHERMAK EXCHANGE; MUSCOVITE; BIOTITE; CHLORITE; KFMASH; CALCULATED MINERAL EQUILIBRIA; PHASE-RELATIONS; SWEDISH-CALEDONIDES; PELITIC SCHISTS; SYSTEM; GEOBAROMETER; SCOTLAND; AUREOLE; FACIES; ROCKS
Identifiers
URN: urn:nbn:se:uu:diva-27999OAI: oai:DiVA.org:uu-27999DiVA: diva2:55895
Note
Addresses: ROOTS M, UPPSALA UNIV, INST EARTH SCI, NORBYVAGEN 18 B, S-75236 UPPSALA, SWEDEN.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-16

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