Crystallographic orientation and geochemical features of mineral inclusions in diamonds

Original language	English
Pages (from-to)	634-649
Number of pages	16
Journal	Russian Geology and Geophysics
Volume	61
Issue number	5-6
DOIs	https://doi.org/10.15372/RGG2020144
Publication status	Published - 1 May 2020

Chromite, Coesite, Diamond, Eclogite, Garnet, Geothermobarometry, High and ultrahigh pressures, High-density fluid inclusions, Inclusion morphology, Mineral equilibria, Olivine, Paragenesis, Peridotite, Relative orientation of diamond and inclusions, eclogite, UDACHNAYA KIMBERLITE PIPE, SIBERIAN DIAMONDS, garnet, olivine, peridotite, high-density fluid inclusions, chromite, mineral equilibria, LITHOSPHERIC MANTLE, high and ultrahigh pressures, MIR KIMBERLITE, ECLOGITE XENOLITHS, FLUID INCLUSIONS, relative orientation of diamond and inclusions, paragenesis, inclusion morphology, diamond, TRACE-ELEMENTS, geothermobarometry, coesite, OLIVINE INCLUSIONS, CARBON-ISOTOPE, ISOTOPIC COMPOSITION

ID: 24895018