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Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure. / Gryaznov, I. A.; Zhimulev, E. I.; Sonin, V. M. и др.

в: Doklady Earth Sciences, Том 489, № 2, 01.12.2019, стр. 1449-1452.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Gryaznov, IA, Zhimulev, EI, Sonin, VM, Lindenblot, ES, Chepurov, AA & Sobolev, NV 2019, 'Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure', Doklady Earth Sciences, Том. 489, № 2, стр. 1449-1452. https://doi.org/10.1134/S1028334X19120122

APA

Gryaznov, I. A., Zhimulev, E. I., Sonin, V. M., Lindenblot, E. S., Chepurov, A. A., & Sobolev, N. V. (2019). Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure. Doklady Earth Sciences, 489(2), 1449-1452. https://doi.org/10.1134/S1028334X19120122

Vancouver

Gryaznov IA, Zhimulev EI, Sonin VM, Lindenblot ES, Chepurov AA, Sobolev NV. Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure. Doklady Earth Sciences. 2019 дек. 1;489(2):1449-1452. doi: 10.1134/S1028334X19120122

Author

Gryaznov, I. A. ; Zhimulev, E. I. ; Sonin, V. M. и др. / Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure. в: Doklady Earth Sciences. 2019 ; Том 489, № 2. стр. 1449-1452.

BibTeX

@article{e435049173ff43859c3755d6b4281a37,
title = "Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure",
abstract = "The primary results are presented on the dissolution of plane-faced diamond crystals of octahedral habit in a Fe–Ni–S melt under 3.5 GPa and 1400°C. It was found that the dissolution resulted in the transformation of plane-faced into curve-faced individuals of morphological features characteristic for kimberlite diamonds. It was concluded that the diamond forms as such might have formed in reduced domains of the Earth{\textquoteright}s mantle before becoming involved in the kimberlite magma.",
keywords = "ORIGIN",
author = "Gryaznov, {I. A.} and Zhimulev, {E. I.} and Sonin, {V. M.} and Lindenblot, {E. S.} and Chepurov, {A. A.} and Sobolev, {N. V.}",
year = "2019",
month = dec,
day = "1",
doi = "10.1134/S1028334X19120122",
language = "English",
volume = "489",
pages = "1449--1452",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Morphological Features of Diamond Crystals Resulting from Dissolution in a Fe–Ni–S Melt under High Pressure

AU - Gryaznov, I. A.

AU - Zhimulev, E. I.

AU - Sonin, V. M.

AU - Lindenblot, E. S.

AU - Chepurov, A. A.

AU - Sobolev, N. V.

PY - 2019/12/1

Y1 - 2019/12/1

N2 - The primary results are presented on the dissolution of plane-faced diamond crystals of octahedral habit in a Fe–Ni–S melt under 3.5 GPa and 1400°C. It was found that the dissolution resulted in the transformation of plane-faced into curve-faced individuals of morphological features characteristic for kimberlite diamonds. It was concluded that the diamond forms as such might have formed in reduced domains of the Earth’s mantle before becoming involved in the kimberlite magma.

AB - The primary results are presented on the dissolution of plane-faced diamond crystals of octahedral habit in a Fe–Ni–S melt under 3.5 GPa and 1400°C. It was found that the dissolution resulted in the transformation of plane-faced into curve-faced individuals of morphological features characteristic for kimberlite diamonds. It was concluded that the diamond forms as such might have formed in reduced domains of the Earth’s mantle before becoming involved in the kimberlite magma.

KW - ORIGIN

UR - http://www.scopus.com/inward/record.url?scp=85081119534&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19120122

DO - 10.1134/S1028334X19120122

M3 - Article

AN - SCOPUS:85081119534

VL - 489

SP - 1449

EP - 1452

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 23759226