| Reference Type | Journal (article/letter/editorial) |
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| Title | The geochemistry of loveringite, a uranium-rare-earth-bearing accessory phase from the Jimberlana Intrusion of Western Australia |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Campbell, I. H. | Author |
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| Kelly, P. R. | Author |
| Year | 1978 (June) | Volume | 42 |
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| Issue | 322 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-322-187.pdf+ |
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| DOI | doi:10.1180/minmag.1978.042.322.04Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2895 | Long-form Identifier | mindat:1:5:2895:4 |
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| GUID | 0 |
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| Full Reference | Campbell, I. H., Kelly, P. R. (1978) The geochemistry of loveringite, a uranium-rare-earth-bearing accessory phase from the Jimberlana Intrusion of Western Australia. Mineralogical Magazine, 42 (322) 187-193 doi:10.1180/minmag.1978.042.322.04 |
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| Plain Text | Campbell, I. H., Kelly, P. R. (1978) The geochemistry of loveringite, a uranium-rare-earth-bearing accessory phase from the Jimberlana Intrusion of Western Australia. Mineralogical Magazine, 42 (322) 187-193 doi:10.1180/minmag.1978.042.322.04 |
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| In | (1978, June) Mineralogical Magazine Vol. 42 (322) Mineralogical Society |
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| Abstract/Notes | SummaryThe distribution and geochemistry of loveringite, an accessory Ti, Fe±Cr oxide containing U and rare-earth elements (Ln) from the Jimberlana Intrusion, have been studied. Loveringite is most abundant in bronzite cumulates; it is found in trace amounts in early plagioclase-augite-hypersthene cumulates, but is not found in the olivine cumulates or in the late-stage differentiates. Loveringites from the bronzite cumulates have a high Cr content compared with those from the plagioclase-augite-hypersthene cumulates, suggesting that the mineral is stabilized by the presence of Cr in the intercumulus liquid. The Ln pattern shows a strong depletion trend from La to Eu, a sharp reversal between Eu and Tb and a second depletion pattern from Tb to Lu. This pattern suggests that the Ln are substituting into two sites, one much larger than the other. |
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