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The incorporation of "water" in a high-pressure 2:1 layer silicate; a high pressure differential thermal analysis of the 10 Aa phase
Anna Kokines Miller, Stephen Guggenheim and August F. Koster van Groos
The incorporation of "water" in a high-pressure 2:1 layer silicate; a high pressure differential thermal analysis of the 10 Aa phase
American Mineralogist (February 1991) 76 (1-2): 106-112
The incorporation of "water" in a high-pressure 2:1 layer silicate; a high pressure differential thermal analysis of the 10 Aa phase
American Mineralogist (February 1991) 76 (1-2): 106-112
Index Terms/Descriptors
Abstract
The 10 Angstrom phase, a talc- and mica-like high-P phase with excess water relative to talc, was investigated using high-P DTA at P to 5.2 kbar, to determine the enthalpy of bonding of the interlayer water species.
ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 76
Serial Issue: 1-2
Title: The incorporation of "water" in a high-pressure 2:1 layer silicate; a high pressure differential thermal analysis of the 10 Aa phase
Affiliation: Univ. Ill. at Chicago, Dep. Geol. Sci.,
Chicago, IL,
United States
Pages: 106-112
Published: 199102
Text Language: English
Publisher: Mineralogical Society of America,
Washington, DC,
United States
References: 29
Accession Number: 1991-032460
Categories: General geophysicsMineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1991
