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High-pressure Al-rich hexagonal phases; what are their kin?
E. Makovicky and L. Arnskov Olsen
High-pressure Al-rich hexagonal phases; what are their kin?
American Mineralogist (October 2008) 93 (10): 1585-1587
High-pressure Al-rich hexagonal phases; what are their kin?
American Mineralogist (October 2008) 93 (10): 1585-1587
Index Terms/Descriptors
Abstract
The hexagonal Al-rich high-pressure phases are members of a structural family with the same type of framework composed of double-ribbons of edge-sharing octahedra, but variably occupied trigonal and hexagonal channels. This family includes jaffeite, fluoborite, yeremeyevite, painite, and synthetic Ba indates. This kinship broadens the spectrum of elements potentially accommodated by these phases in the mantle.
ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 93
Serial Issue: 10
Title: High-pressure Al-rich hexagonal phases; what are their kin?
Affiliation: University of Copenhagen, Department of Geography and Geology,
Copenhagen,
Denmark
Affiliation: University of Toronto, Department of Geology,
Toronto, ON,
Canada
Pages: 1585-1587
Published: 200810
Text Language: English
Publisher: Mineralogical Society of America,
Washington, DC,
United States
References: 15
DOI:
10.2138/am.2008.2859
Accession Number: 2009-001470
Categories: Geophysics of minerals and rocks
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. table
Secondary Affiliation: CNRS-IPGP,
FRA,
France
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, Mineralogical Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 200901
