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Korolev, N.M., Kopylova, M., Bussweiler, Y., Pearson, D.G., Gurney, J., Davidson, J. (2018) The uniquely high-temperature character of Cullinan diamonds: A signature of the Bushveld mantle plume?. Lithos, 304. 362-373 doi:10.1016/j.lithos.2018.02.011

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Reference TypeJournal (article/letter/editorial)
TitleThe uniquely high-temperature character of Cullinan diamonds: A signature of the Bushveld mantle plume?
JournalLithos
AuthorsKorolev, N.M.Author
Kopylova, M.Author
Bussweiler, Y.Author
Pearson, D.G.Author
Gurney, J.Author
Davidson, J.Author
Year2018 (April)Volume304
Page(s)362-373
PublisherElsevier BV
DOIdoi:10.1016/j.lithos.2018.02.011Search in ResearchGate
Mindat Ref. ID277516Long-form Identifiermindat:1:5:277516:0
GUID2f52d0c6-4b03-4ff6-b7ca-6bec2ee0ca98
Full ReferenceKorolev, N.M., Kopylova, M., Bussweiler, Y., Pearson, D.G., Gurney, J., Davidson, J. (2018) The uniquely high-temperature character of Cullinan diamonds: A signature of the Bushveld mantle plume?. Lithos, 304. 362-373 doi:10.1016/j.lithos.2018.02.011
Plain TextKorolev, N.M., Kopylova, M., Bussweiler, Y., Pearson, D.G., Gurney, J., Davidson, J. (2018) The uniquely high-temperature character of Cullinan diamonds: A signature of the Bushveld mantle plume?. Lithos, 304. 362-373 doi:10.1016/j.lithos.2018.02.011
In(2018) Lithos Vol. 304. Elsevier BV

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Danchin (1979) Mineral and bulk chemistry of garnet lherzolite and garnet harzburgite xenoliths from the Premier Mine, South Africa , 104
Gurney (1985) South African Journal of Geology Inclusions in Premier mine diamonds 88, 301
Tsai (1979) Mineral Inclusions in Diamond: Premier, Jagersfontein and Finsch Kimberlites, South Africa, and Williamson Mine, Tanzania 15, 16
Wang (1993) American Mineralogist Micro-Raman and infrared spectral study of forsterite under high pressure 78, 469


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