Diamond growth from oxidized carbon sources beneath the Northern Slave Craton, Canada: A δ13C–N study of eclogite-hosted diamonds from the Jericho kimberlite-Reference-Cited by-同舟云学术

Diamond growth from oxidized carbon sources beneath the Northern Slave Craton, Canada: A δ13C–N study of eclogite-hosted diamonds from the Jericho kimberlite

Published:2011-10 Issue:20 Volume:75 Page:6027-6047
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Smart Katie A.,Chacko Thomas,Stachel Thomas,Muehlenbachs Karlis,Stern Richard A.,Heaman Larry M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference86 articles.

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

4. Infrared absorption by the B nitrogen aggregate in diamond;Boyd;Philos. Mag. B,1995

5. Luminescence of diamonds from metamorphic rocks;Bruce;Am. Mineral.,2011

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