| Reference Type | Journal (article/letter/editorial) |
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| Title | Preliminary fluid inclusion studies in a high-grade blueschist terrain, Syros, Greece |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Barr, Hazel | Author |
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| Year | 1990 (June) | Volume | 54 |
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| Issue | 375 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_54/54-375-159.pdf+ |
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| DOI | doi:10.1180/minmag.1990.054.375.03Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 1605 | Long-form Identifier | mindat:1:5:1605:0 |
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| GUID | 0 |
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| Full Reference | Barr, Hazel (1990) Preliminary fluid inclusion studies in a high-grade blueschist terrain, Syros, Greece. Mineralogical Magazine, 54 (375) 159-168 doi:10.1180/minmag.1990.054.375.03 |
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| Plain Text | Barr, Hazel (1990) Preliminary fluid inclusion studies in a high-grade blueschist terrain, Syros, Greece. Mineralogical Magazine, 54 (375) 159-168 doi:10.1180/minmag.1990.054.375.03 |
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| In | (1990, June) Mineralogical Magazine Vol. 54 (375) Mineralogical Society |
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| Abstract/Notes | AbstractPreliminary fluid inclusion measurements have been made on quartz (whole rocks and segregations) and garnet from a blueschist terrain. Although further measurements are required, the fluids apparently associated with the blueschist event are aqueous with no thermometrically detectable CO2, a feature which is consistent with mineral-fluid equilibria studies. The salinity of the fluid inclusions is highly variable, from almost pure H2O to halite saturation, and a mechanism involving hydration reactions, such as proposed by Crawford et al. (1979), is suggested. Fluid inclusions associated with the greenschist overprint, which has affected the terrain, are also aqueous in nature. |
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These are possibly similar items as determined by title/reference text matching only.
