Инд. авторы:	Zhimulev E.I, Sonin V.M., Afanasiev V.P., Chepurov A.I., Pokhilenko N.P.
Заглавие:	Fe–S melt as a likely solvent of diamond under mantle conditions
Библ. ссылка:	Zhimulev E.I, Sonin V.M., Afanasiev V.P., Chepurov A.I., Pokhilenko N.P. Fe–S melt as a likely solvent of diamond under mantle conditions // Doklady Earth Sciences. - 2016. - Vol.471. - Iss. 2. - P.1277-1279. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X16120163; SCOPUS: 2-s2.0-85008655923; WoS: 000392141700014;
Реферат:	eng: 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. © 2016, Pleiades Publishing, Ltd.
Ключевые слова:	T parameter; nocv1; Natural diamonds; Diamonds; Experimental conditions; Diamond crystals; Earth sciences; Morphological features;
Издано:	2016
Физ. характеристика:	с.1277-1279