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Enami, Masaki, Banno, Shohei (1980) Zoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications. Mineralogical Magazine, 43 (332) 1005-1013 doi:10.1180/minmag.1980.043.332.08

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Reference TypeJournal (article/letter/editorial)
TitleZoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications
JournalMineralogical MagazineISSN0026-461X
AuthorsEnami, MasakiAuthor
Banno, ShoheiAuthor
Year1980 (December)Volume43
Issue332
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_43/43-332-1005.pdf+
DOIdoi:10.1180/minmag.1980.043.332.08Search in ResearchGate
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Mindat Ref. ID3189Long-form Identifiermindat:1:5:3189:3
GUID0
Full ReferenceEnami, Masaki, Banno, Shohei (1980) Zoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications. Mineralogical Magazine, 43 (332) 1005-1013 doi:10.1180/minmag.1980.043.332.08
Plain TextEnami, Masaki, Banno, Shohei (1980) Zoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications. Mineralogical Magazine, 43 (332) 1005-1013 doi:10.1180/minmag.1980.043.332.08
In(1980, December) Mineralogical Magazine Vol. 43 (332) Mineralogical Society
Abstract/NotesSummaryCoexisting zoisite and clinozoisite in seventeen specimens from six localities in Japan have been studied with the electron-probe microanalyser. Zoisite and clinozoisite are commonly zoned, but compositional gaps between them are systematic. Referring to the metamorphic grade of the host rocks, a temporary and schematic phase-diagram for the system Ca2Al3Si3O12-(OH)-Ca2Al2Fe3+Si3O12(OH) is presented. With increasing temperature, in the range of low- to medium-grade metamorphism, the compositional gap between the two epidote-group minerals shifts towards higher Fe3+ compositions.


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