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Fe–S melt as a likely solvent of diamond under mantle conditions. / Zhimulev, E. I.; Sonin, V. M.; Afanasiev, V. P. et al.

In: Doklady Earth Sciences, Vol. 471, No. 2, 01.12.2016, p. 1277-1279.

Research output: Contribution to journal › Article › peer-review

Harvard

Zhimulev, EI, Sonin, VM, Afanasiev, VP, Chepurov, AI & Pokhilenko, NP 2016, 'Fe–S melt as a likely solvent of diamond under mantle conditions', Doklady Earth Sciences, vol. 471, no. 2, pp. 1277-1279. https://doi.org/10.1134/S1028334X16120163

APA

Zhimulev, E. I., Sonin, V. M., Afanasiev, V. P., Chepurov, A. I., & Pokhilenko, N. P. (2016). Fe–S melt as a likely solvent of diamond under mantle conditions. Doklady Earth Sciences, 471(2), 1277-1279. https://doi.org/10.1134/S1028334X16120163

Vancouver

Zhimulev EI, Sonin VM, Afanasiev VP, Chepurov AI, Pokhilenko NP. Fe–S melt as a likely solvent of diamond under mantle conditions. Doklady Earth Sciences. 2016 Dec 1;471(2):1277-1279. doi: 10.1134/S1028334X16120163

Author

Zhimulev, E. I. ; Sonin, V. M. ; Afanasiev, V. P. et al. / Fe–S melt as a likely solvent of diamond under mantle conditions. In: Doklady Earth Sciences. 2016 ; Vol. 471, No. 2. pp. 1277-1279.

BibTeX

@article{e214c0e0364c43e5ad985120b95f20bc,
title = "Fe–S melt as a likely solvent of diamond under mantle conditions",
abstract = "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.",
author = "Zhimulev, {E. I.} and Sonin, {V. M.} and Afanasiev, {V. P.} and Chepurov, {A. I.} and Pokhilenko, {N. P.}",
year = "2016",
month = dec,
day = "1",
doi = "10.1134/S1028334X16120163",
language = "English",
volume = "471",
pages = "1277--1279",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

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