Reference Type | Journal (article/letter/editorial) |
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Title | Zoisite-clinozoisite relations in low- to medium-grade high-pressure metamorphic rocks and their implications |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Enami, Masaki | Author |
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Banno, Shohei | Author |
Year | 1980 (December) | Volume | 43 |
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Issue | 332 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-332-1005.pdf+ |
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DOI | doi:10.1180/minmag.1980.043.332.08Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 3189 | Long-form Identifier | mindat:1:5:3189:3 |
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GUID | 0 |
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Full Reference | 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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Plain Text | 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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In | (1980, December) Mineralogical Magazine Vol. 43 (332) Mineralogical Society |
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Abstract/Notes | SummaryCoexisting 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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