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The formation of pigeonite on the join hedenbergite-ferrosilite at 11.5 and 15 kbar; experiments and a solution model

Donald H. Lindsley
The formation of pigeonite on the join hedenbergite-ferrosilite at 11.5 and 15 kbar; experiments and a solution model
American Mineralogist (December 1981) 66 (11-12): 1175-1182

Abstract

The thermodynamics and experimental data are discussed. Apparently this join at high P is directly applicable to crustal rocks such as the Skaergaard intrusion and a number of lunar basalts which have been extremely enriched with Fe.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 66
Serial Issue: 11-12
Title: The formation of pigeonite on the join hedenbergite-ferrosilite at 11.5 and 15 kbar; experiments and a solution model
Author(s): Lindsley, Donald H.
Affiliation: State Univ. N.Y., Dep. Earth and Planet. Sci., Stony Brook, NY, United States
Pages: 1175-1182
Published: 198112
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 20
Accession Number: 1982-032709
Categories: Geophysics of minerals and rocks
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 3 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1982
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