Type IIa diamond formation

The petrological model of type IIa diamond formation is proposed. By the model these diamonds were formed from fluids on the last stages of kimberlite magma formation at 600-700 C and 20-30 kbar. The model explains the main specific of the type IIa diamonds. They are the enrichment of light carbon, low nitrogen content, the absence of silicate inclusions, the large size and cleanliness, a high degree of desorption, association with the products of late crystallization of kimberlite magmas.

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12.11.2018

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12.11.2018

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GOST	Simakov S. Type IIa diamond formation // Doklady Akademii nauk – 2018. – V. 482. – Issue 5 C. 583-586 [Electronic resource]. URL: http://ras.jes.su/dan/s086956520003037-3-1-en (circulation date: 25.04.2024). DOI: 10.31857/S086956520003037-3
MLA	Simakov, Sergey "Type IIa diamond formation." Doklady Akademii nauk 482.5 (2018):583-586. DOI: 10.31857/S086956520003037-3
APA	Simakov S. (2018). Type IIa diamond formation. Doklady Akademii nauk 482(5), pp.583-586 DOI: 10.31857/S086956520003037-3

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