Micron-scale δ<sup>13</sup>C determination by NanoSIMS in a Juina diamond with a carbonate inclusion-Reference-Cited by-同舟云学术

Micron-scale δ¹³C determination by NanoSIMS in a Juina diamond with a carbonate inclusion

Published:2016-07-29 Issue:4 Volume:50 Page:e7-e12
ISSN:0016-7002
Container-title:GEOCHEMICAL JOURNAL
language:en
Short-container-title:Geochem. J.

Author:

Pinti Daniele L.¹,Ishida Akizumi²,Takahata Naoto²,Sano Yuji²,Bureau Hélène³,Cartigny Pierre⁴

Affiliation:

1. GEOTOP and Département des sciences de la Terre et de l’atmosphère, Université du Québec à Montréal

2. Atmosphere and Ocean Research Institute, The University of Tokyo

3. Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Sorbonne Universités - UPMC Univ. Paris 06, CNRS UMR 7590 & Muséum National d’Histoire Naturelle

4. Laboratoire de Géochimie des Isotopes Stables, Institut de Physique du Globe de Paris, Université Paris Diderot, CNRS

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Link

https://www.jstage.jst.go.jp/article/geochemj/50/4/50_2.0427/_pdf

Reference38 articles.

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2. Brenker, F. E., Vollmer, C., Vincze, L., Vekemans, B., Szymanski, A., Janssens, K., Szaloki, I., Nasdala, L., Joswig, W. and Kaminsky, F. (2007) Carbonates from the lower part of transition zone or even the lower mantle. Earth Planet. Sci. Lett. 260, 1–9.

3. Bulanova, G. P., Walter, M. J., Smith, C. B., Kohn, S. C., Amstrong, L. S., Blundy, J. and Gobbo, L. (2010) Mineral inclusions in sublithospheric diamonds from Collier 4 kimberlite pipe, Juina, Brazil: subducted protoliths, carbonated melts and primary kimberlite magmatism. Contrib. Mineral. Petrol. 160, 489–510.

4. Bureau, H., Langenhorst, F., Auzende, A.-L., Frost, D. J., Estève, I. and Siebert, J. (2012) The growth of fibrous, cloudy and polycrystalline diamonds. Geochim. Cosmochim. Acta 77, 202–214.

5. Cartigny, P. (2005) Stable isotopes and the origin of diamond. Elements 1, 79–84.

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