Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Fe–S melt as a likely solvent of diamond under mantle conditions. / Zhimulev, E. I.; Sonin, V. M.; Afanasiev, V. P. и др.
в: Doklady Earth Sciences, Том 471, № 2, 01.12.2016, стр. 1277-1279.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Fe–S melt as a likely solvent of diamond under mantle conditions
AU - Zhimulev, E. I.
AU - Sonin, V. M.
AU - Afanasiev, V. P.
AU - Chepurov, A. I.
AU - Pokhilenko, N. P.
PY - 2016/12/1
Y1 - 2016/12/1
N2 - The first results of experimental study of diamond dissolution in a S-bearing Fe melt at high P–T parameters are reported and the morphology of partially dissolved crystals is compared with that of natural diamonds. Our results show that under the experimental conditions (4 GPa, 1400°C), flat-faced octahedral diamond crystals are transformed into curve-faced octahedroids with morphological features similar to those of natural diamonds.
AB - The first results of experimental study of diamond dissolution in a S-bearing Fe melt at high P–T parameters are reported and the morphology of partially dissolved crystals is compared with that of natural diamonds. Our results show that under the experimental conditions (4 GPa, 1400°C), flat-faced octahedral diamond crystals are transformed into curve-faced octahedroids with morphological features similar to those of natural diamonds.
UR - http://www.scopus.com/inward/record.url?scp=85008655923&partnerID=8YFLogxK
U2 - 10.1134/S1028334X16120163
DO - 10.1134/S1028334X16120163
M3 - Article
AN - SCOPUS:85008655923
VL - 471
SP - 1277
EP - 1279
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -
ID: 25755380