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Formation and evolution of hypabyssal kimberlites from the Siberian craton: Part 1 – New insights from cathodoluminescence of the carbonates
Research output
:
Contribution to journal
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Article
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peer-review
Section of General and Regional Geology
Laboratory for Experimental Geochemistry and Petrology of the Earth's Mantle
Overview
Cite this
DOI
https://doi.org/10.1016/j.jseaes.2017.06.009
Final published version
N. V. Sobolev
H. P. Schertl
R. D. Neuser
A. A. Tomilenko
D. V. Kuzmin
A. M. Logvinova
A. V. Tolstov
S. I. Kostrovitsky
D. A. Yakovlev
O. B. Oleinikov
Original language
English
Pages (from-to)
670-678
Number of pages
9
Journal
Journal of Asian Earth Sciences
Volume
145
DOIs
https://doi.org/10.1016/j.jseaes.2017.06.009
Publication status
Published -
1 Sept 2017
OECD FOS+WOS
Research areas
Carbonate, Carbonatite, Cathodoluminescence, Hypabyssal, Kimberlite, Siberian craton, CRYSTALLIZATION, MINERALS, OXYGEN-ISOTOPE, UHP-METAMORPHIC ROCKS, U-PB, TRACE-ELEMENT, JADEITITE, YAKUTIAN KIMBERLITES, KOKCHETAV MASSIF, DIAMOND FORMATION
ID: 9981332