Abstract
Three single crystals of clinopyroxene trapped within three different gem-quality diamonds from the Udachnaya kimberlite (Siberia, Russia) were analysed in situ by single-crystal synchrotron X-ray diffraction in order to obtain information on their chemical composition and infer source assemblage type. A non-destructive approach was used with high-energy (≈ 60 keV; λ ≈ 0.206 Å) at I15, the extreme-conditions beamline at Diamond Light Source. A dedicated protocol was used to center the mineral inclusions located deep inside the diamonds in the X-ray beam. Our results reveal that two of the inclusions can be associated with peridotitic paragenesis whereas the third is eclogitic. This study also demonstrates that this non-destructive experimental approach is extremely efficient in evaluating the origin of minerals trapped in their diamond hosts.
Original language | English |
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Pages (from-to) | 334-338 |
Number of pages | 5 |
Journal | LITHOS |
Volume | 265 |
DOIs | |
Publication status | Published - Nov 15 2016 |
Keywords
- Clinopyroxene
- Diamond
- Eclogite
- Peridotite
- Synchrotron
ASJC Scopus subject areas
- Geology
- Geochemistry and Petrology