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==Further reading== {{refbegin}} * {{cite book |title=Petrology of Lamproites |last=Mitchell |first=R. H. |author2=Bergman, S. C. |year=1991 |publisher=Plenum Press |location=New York |isbn=978-0-306-43556-0 }} * Edwards, C. B., Howkins, J. B., 1966. Kimberlites in Tanganyika with special reference to the Mwadui occurrence. Econ. Geol., 61:537-554. * {{cite web|last1=Kopylova|first1=Maya G.|title=Definition of Kimberlite|url=https://www.eoas.ubc.ca/research/diamonds/kopylova/intro/definition.html|website=Diamond Exploration Laboratory|publisher=University of British Columbia|access-date=30 August 2017}} * Nixon, P. H., 1995. The morphology and nature of primary diamondiferous occurrences. Journal of Geochemical Exoloration, 53: 41β71. * {{cite book|last1=Pell|first1=Jennifer|chapter=Kimberlite-hosted Diamonds|chapter-url=http://www.unalmed.edu.co/~rrodriguez/MODELOS/columbia/KIMBERLITE-HOSTED%20DIAMONDS.htm|title=Geological Fieldwork 1997. Paper 1998-1|pages=24Lβ1–24Lβ4|publisher=British Columbia Ministry of Employment and Investment|access-date=30 August 2017|url-status=dead|archive-url=https://web.archive.org/web/20160404230700/http://www.unalmed.edu.co/~rrodriguez/MODELOS/columbia/KIMBERLITE-HOSTED%20DIAMONDS.htm|archive-date=4 April 2016}} * Woolley, A. R., Bergman, S. C., Edgar, A. D., Le Bas, M. J., Mitchell, R. H., Rock, N. M. S., Scott Smith, B. H., 1996. Classification of lamprophyres, lamproites, kimberlites, and the kalsilitic, melilitic, and leucitic rocks. ''The Canadian Mineralogist'', Vol 34, Part 2. pp. 175β186. * {{cite web|url=https://science.ubc.ca/news/geologists-find-lost-fragment-ancient-continent-canada%E2%80%99s-north|author=Kopylova|title=Geologists find lost fragment of ancient continent in Canada's North. See the interesting citation from the main author: "For researchers, kimberlites are subterranean rockets that pick up passengers on their way to the surface," explains University of British Columbia geologist Maya Kopylova. "The passengers are solid chunks of wall rocks that carry a wealth of details on conditions far beneath the surface of our planet over time."|date=19 March 2020|work=science.ubc.ca|access-date=21 March 2020}} {{refend}}
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