| Reference Type | Journal (article/letter/editorial) |
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| Title | Iron oxide mineralogy of a hydrothermal assemblage on Santorini Island, Aegean Sea |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Murad, Enver | Author |
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| Year | 1982 (March) | Volume | 46 |
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| Issue | 338 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_46/46-338-89.pdf+ |
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| DOI | doi:10.1180/minmag.1982.046.338.14Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3359 | Long-form Identifier | mindat:1:5:3359:0 |
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| GUID | 0 |
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| Full Reference | Murad, Enver (1982) Iron oxide mineralogy of a hydrothermal assemblage on Santorini Island, Aegean Sea. Mineralogical Magazine, 46 (338) 89-93 doi:10.1180/minmag.1982.046.338.14 |
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| Plain Text | Murad, Enver (1982) Iron oxide mineralogy of a hydrothermal assemblage on Santorini Island, Aegean Sea. Mineralogical Magazine, 46 (338) 89-93 doi:10.1180/minmag.1982.046.338.14 |
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| In | (1982, March) Mineralogical Magazine Vol. 46 (338) Mineralogical Society |
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| Abstract/Notes | AbstractBasement rocks of Santorini have been locally impregnated by iron oxides and other minerals. The hydrothermal fluids which caused the mineralization have extensively altered the impregnated rocks, but left granditic garnets in these unaffected.Mössbauer spectroscopy and differential X-ray diffraction show that the iron oxides present are goethite and hematite in a ratio of about 2 : 1. The presence of hematite indicates that these minerals formed, directly from a hydrothermal phase, at higher temperatures than the recent submarine iron oxide deposits of Santorini, which contain no hematite. |
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