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Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth. / Chepurov, A. I.; Zhimulev, E. I.; Sonin, V. M. et al.

In: Doklady Earth Sciences, Vol. 480, No. 2, 01.06.2018, p. 823-825.

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

Harvard

Chepurov, AI, Zhimulev, EI, Sonin, VM, Tomilenko, AA & Pokhilenko, NP 2018, 'Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth', Doklady Earth Sciences, vol. 480, no. 2, pp. 823-825. https://doi.org/10.1134/S1028334X18060223

APA

Chepurov, A. I., Zhimulev, E. I., Sonin, V. M., Tomilenko, A. A., & Pokhilenko, N. P. (2018). Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth. Doklady Earth Sciences, 480(2), 823-825. https://doi.org/10.1134/S1028334X18060223

Vancouver

Chepurov AI, Zhimulev EI, Sonin VM, Tomilenko AA, Pokhilenko NP. Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth. Doklady Earth Sciences. 2018 Jun 1;480(2):823-825. doi: 10.1134/S1028334X18060223

Author

Chepurov, A. I. ; Zhimulev, E. I. ; Sonin, V. M. et al. / Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth. In: Doklady Earth Sciences. 2018 ; Vol. 480, No. 2. pp. 823-825.

BibTeX

@article{4f2edebd0f334808b48cde06941272b5,
title = "Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth",
abstract = "The first results are presented for the synthesis of diamond at 6.5 GPa and 1600°C during migration of molten iron through a silicate matrix, which is composed of olivine crystals with interstitial graphite. The experiment shows that diamonds in the Earth{\textquoteright}s mantle and the terrestrial planets could have formed during differentiation. Diamond crystals, which were formed during iron segregation of the Earth{\textquoteright}s differentiation, could be centers for further crystallization of mantle diamonds.",
keywords = "CATALYZED HYDROGENATION, IRON PARTICLES, MOLTEN IRON, INCLUSIONS, GRAPHITE, CARBON",
author = "Chepurov, {A. I.} and Zhimulev, {E. I.} and Sonin, {V. M.} and Tomilenko, {A. A.} and Pokhilenko, {N. P.}",
year = "2018",
month = jun,
day = "1",
doi = "10.1134/S1028334X18060223",
language = "English",
volume = "480",
pages = "823--825",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Experimental Test of Possible Formation of Diamond under the Differentiation of the Earth

AU - Chepurov, A. I.

AU - Zhimulev, E. I.

AU - Sonin, V. M.

AU - Tomilenko, A. A.

AU - Pokhilenko, N. P.

PY - 2018/6/1

Y1 - 2018/6/1

N2 - The first results are presented for the synthesis of diamond at 6.5 GPa and 1600°C during migration of molten iron through a silicate matrix, which is composed of olivine crystals with interstitial graphite. The experiment shows that diamonds in the Earth’s mantle and the terrestrial planets could have formed during differentiation. Diamond crystals, which were formed during iron segregation of the Earth’s differentiation, could be centers for further crystallization of mantle diamonds.

AB - The first results are presented for the synthesis of diamond at 6.5 GPa and 1600°C during migration of molten iron through a silicate matrix, which is composed of olivine crystals with interstitial graphite. The experiment shows that diamonds in the Earth’s mantle and the terrestrial planets could have formed during differentiation. Diamond crystals, which were formed during iron segregation of the Earth’s differentiation, could be centers for further crystallization of mantle diamonds.

KW - CATALYZED HYDROGENATION

KW - IRON PARTICLES

KW - MOLTEN IRON

KW - INCLUSIONS

KW - GRAPHITE

KW - CARBON

UR - http://www.scopus.com/inward/record.url?scp=85050096594&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18060223

DO - 10.1134/S1028334X18060223

M3 - Article

AN - SCOPUS:85050096594

VL - 480

SP - 823

EP - 825

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25754992