Diamond growth from C–H–N–O recycled fluids in the lithosphere: Evidence from CH 4 micro-inclusions and δ 13 C– δ 15 N–N content in Marange mixed-habit diamonds

Author:

Smit Karen V.,Shirey Steven B.,Stern Richard A.,Steele Andrew,Wang Wuyi

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference114 articles.

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2. The Fe3+/ΣFe ratios or MORB glasses and their implications for mantle melting;Bezos;Geochimica et Cosmochimica Acta,2005

3. The relationship between infrared absorption and the A defect concentration in diamond;Boyd;Philosophical Magazine B,1994

4. Infrared absorption by the B nitrogen aggregate in diamond;Boyd;Philosophical Magazine B,1995

5. Carbon and nitrogen isotope systematics within a sector-growth diamond from the Mir kimberlite, Yakutia;Bulanova;Chemical Geology,2002

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