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SIGNIFICANCE OF THE ASSEMBLAGE TITANITE * MAGNETITE * QUARTZ IN GRANITIC ROCKS (1989)
The equilibrium hedenbergite + ilmenite + oxygen : titanite + magrretite * quartz isimportant in distinguishing relatively oxidized from relatively reduced granitic rocks. This study deals with the aforementioned.
Reference:
American Mineralogist, Volume 74, pages 744-749, 1989
American Mineralogist, Volume 74, pages 744-749, 1989
Organization:
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061, U.S.A.
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061, U.S.A.
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