Carbon and Nitrogen in Mantle-Derived Diamonds-Reference-Cited by-同舟云学术

Carbon and Nitrogen in Mantle-Derived Diamonds

Published:2022-07-01 Issue:1 Volume:88 Page:809-875
ISSN:1529-6466
Container-title:Reviews in Mineralogy and Geochemistry
language:en
Short-container-title:

Author:

Stachel Thomas¹,Cartigny Pierre²,Chacko Thomas¹,Pearson D. Graham¹

Affiliation:

1. Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T6G 2E3, Canada

2. Institut de physique du globe de Paris, Université de Paris, CNRS, F-75005 Paris, France

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology

Link

https://pubs.geoscienceworld.org/msa/rimg/article-pdf/88/1/809/5645162/rmg.2022.88.15.pdf

Reference276 articles.

1. The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth’s mantle;Adam;Geochem Geophys Geosystems,2014

2. Isotopic and elemental evidence for a relationship between kimberlite and Zaire cubic diamonds;Akagi;Nature,1988

3. Appora-Gnekindy I (1998) Etude expérimentale du fractionnement isotopique du carbone et de l’oxygène dans les systèmes CO2–carbonate liquides: Application aux contextes carbonatiques. PhD thesis, Institut de Physique du Globe de Paris, 351p

4. Carbon and hydrogen isotope constraints on degassing of CO2 and H2O in submarine lavas from the Pitcairn hotspot (South Pacific);Aubaud;Geophys Res Lett,2006

5. Diamond ages from Victor (Superior Craton): Intra-mantle cycling of volatiles (C, N, S) during supercontinent reorganisation;Aulbach;Earth Planet Sci Lett,2018

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