Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Typomorphic features of graphite inclusions in diamond : Experimental data. / Khokhryakov, A. F.; Nechaev, D. V.
в: Russian Geology and Geophysics, Том 56, № 1-2, 01.01.2015, стр. 232-238.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Typomorphic features of graphite inclusions in diamond
T2 - Experimental data
AU - Khokhryakov, A. F.
AU - Nechaev, D. V.
PY - 2015/1/1
Y1 - 2015/1/1
N2 - Diamond crystals with graphite inclusions synthesized during the experimental modeling of natural diamond formation in chloride and carbonate systems under mantle PT-conditions were studied to elucidate the specifics of the protogenetic graphite inclusions. It has been established that the inclusions of graphite, both primary ones and those resulted from sodium oxalate decomposition, form compact clusters of grains and plates of different shapes in diamond. Diamonds rich in graphite inclusions are black and opaque. Their distinctive feature is significant low-frequency shift (to 1328cm-1) and broadening (to 6.5cm-1) of the Raman line, testifying to high residual deformation. Based on the data of previous experiments and the results obtained in this study, we consider peculiarities of protogenetic, syngenetic, and epigenetic graphite inclusions in diamond and their possible use as typomorphic features for the investigation of natural diamonds and reconstruction of their genesis.
AB - Diamond crystals with graphite inclusions synthesized during the experimental modeling of natural diamond formation in chloride and carbonate systems under mantle PT-conditions were studied to elucidate the specifics of the protogenetic graphite inclusions. It has been established that the inclusions of graphite, both primary ones and those resulted from sodium oxalate decomposition, form compact clusters of grains and plates of different shapes in diamond. Diamonds rich in graphite inclusions are black and opaque. Their distinctive feature is significant low-frequency shift (to 1328cm-1) and broadening (to 6.5cm-1) of the Raman line, testifying to high residual deformation. Based on the data of previous experiments and the results obtained in this study, we consider peculiarities of protogenetic, syngenetic, and epigenetic graphite inclusions in diamond and their possible use as typomorphic features for the investigation of natural diamonds and reconstruction of their genesis.
KW - Diamond
KW - Experiment
KW - Graphite inclusions
KW - Typomorphic features
UR - http://www.scopus.com/inward/record.url?scp=84925299924&partnerID=8YFLogxK
U2 - 10.1016/j.rgg.2015.01.016
DO - 10.1016/j.rgg.2015.01.016
M3 - Article
AN - SCOPUS:84925299924
VL - 56
SP - 232
EP - 238
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 1-2
ER -
ID: 25772761