| Reference Type | Journal (article/letter/editorial) |
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| Title | Natural and laboratory α-particle irradiation of diamond |
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| Journal | Mineralogical Magazine |
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| Authors | Vance, E. R. | Author |
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| Milledge, H. J. | Author |
| Year | 1972 (September) | Volume | 38 |
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| Issue | 299 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-299-878.pdf+ |
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| DOI | doi:10.1180/minmag.1972.038.299.11Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6591 | Long-form Identifier | mindat:1:5:6591:1 |
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| GUID | 0 |
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| Full Reference | Vance, E. R., Milledge, H. J. (1972) Natural and laboratory α-particle irradiation of diamond. Mineralogical Magazine, 38 (299) 878-881 doi:10.1180/minmag.1972.038.299.11 |
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| Plain Text | Vance, E. R., Milledge, H. J. (1972) Natural and laboratory α-particle irradiation of diamond. Mineralogical Magazine, 38 (299) 878-881 doi:10.1180/minmag.1972.038.299.11 |
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| In | (1972, September) Mineralogical Magazine Vol. 38 (299) Mineralogical Society |
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| Abstract/Notes | SummaryTo produce a lattice expansion readily detectable by conventional X-ray photographic means in α-irradiated diamond, a dose of order 1018α.cm−2 is required. Such a dose could be produced by pitchblende in ∼2 × 108 yr. and a previously reported lattice expansion in a natural diamond could therefore have occurred by long-term contact with a radioactive material. α-particle doses greater than ∼1014 cm−2 produce observable green colouration on the surface of an initially colourless diamond. |
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