Reference Type | Journal (article/letter/editorial) |
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Title | Geochemical relationships between some pallasites and iron meteorites |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Scott, Edward R. D. | Author |
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Year | 1977 (June) | Volume | 41 |
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Issue | 318 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_41/41-318-265.pdf+ |
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DOI | doi:10.1180/minmag.1977.041.318.15Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 2768 | Long-form Identifier | mindat:1:5:2768:1 |
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GUID | 0 |
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Full Reference | Scott, Edward R. D. (1977) Geochemical relationships between some pallasites and iron meteorites. Mineralogical Magazine, 41 (318) 265-272 doi:10.1180/minmag.1977.041.318.15 |
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Plain Text | Scott, Edward R. D. (1977) Geochemical relationships between some pallasites and iron meteorites. Mineralogical Magazine, 41 (318) 265-272 doi:10.1180/minmag.1977.041.318.15 |
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In | (1977, June) Mineralogical Magazine Vol. 41 (318) Mineralogical Society |
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Abstract/Notes | SummaryPublished analyses for 14 trace and minor siderophilic elements have been interpreted to indicate a close relationship between the IIIAB iron meteorites and the main group of pallasites. These two groups respectively account for about 32 and 75 % of all irons and pallasites. The composition of the metal in the main group pallasites is very close to that calculated for the liquid after 80 % of a IIIAB iron melt has fractionally crystallized. The pallasites probably formed by the intrusion of residual molten metal from the core into a surrounding olivine mantle. |
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