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GEOREF RECORD

Phase relations of orthopyroxene, olivine, and grunerite in high-grade metamorphic iron-formation

Takashi Miyano and Cornelis Klein
Phase relations of orthopyroxene, olivine, and grunerite in high-grade metamorphic iron-formation
American Mineralogist (August 1983) 68 (7-8): 699-716

Abstract

S degrees (sub 298) , Delta H degrees (sub f,298) , and Delta G degrees (sub f.298) of ferrosilite are 93.05+ or -0.3J/mol . K, -1194.872+ or -1.0kJ/mol, -1117.124+ or -1.0 kJ/mol; those of grunerite 721.8+ or -10.0 J/mol . K, -9648.304+ or - kJ/mol (minimum), and -8988.759+ or -20 kJ/mol (minimum). Phase relations for iron formations classified into three types: (I) olivine-free, (II) olivine- and quartz-bearing, and (III) olivine-bearing and quartz-free relations. Each type may or may not include grunerite; its presence is strongly influenced by the magnitude of fH (sub 2) O.The formation of retrograde grunerite appears to be dependent upon fH (sub 2) O rather than on the lowering of T.--Modified journal abstract.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 68
Serial Issue: 7-8
Title: Phase relations of orthopyroxene, olivine, and grunerite in high-grade metamorphic iron-formation
Affiliation: Indiana Univ., Dep. Geol., Bloomington, IN, United States
Pages: 699-716
Published: 198308
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 76
Accession Number: 1984-002316
Categories: Igneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 6 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute.
Update Code: 1984
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