Standard

Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition. / Chepurov, A. I.; Tomilenko, A. A.; Sonin, V. M. et al.

In: Doklady Earth Sciences, Vol. 492, No. 1, 01.05.2020, p. 333-337.

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

Harvard

Chepurov, AI, Tomilenko, AA, Sonin, VM, Zhimulev, EI, Bul’bak, TA, Chepurov, AA & Sobolev, NV 2020, 'Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition', Doklady Earth Sciences, vol. 492, no. 1, pp. 333-337. https://doi.org/10.1134/S1028334X20050050

APA

Chepurov, A. I., Tomilenko, A. A., Sonin, V. M., Zhimulev, E. I., Bul’bak, T. A., Chepurov, A. A., & Sobolev, N. V. (2020). Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition. Doklady Earth Sciences, 492(1), 333-337. https://doi.org/10.1134/S1028334X20050050

Vancouver

Chepurov AI, Tomilenko AA, Sonin VM, Zhimulev EI, Bul’bak TA, Chepurov AA et al. Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition. Doklady Earth Sciences. 2020 May 1;492(1):333-337. doi: 10.1134/S1028334X20050050

Author

Chepurov, A. I. ; Tomilenko, A. A. ; Sonin, V. M. et al. / Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition. In: Doklady Earth Sciences. 2020 ; Vol. 492, No. 1. pp. 333-337.

BibTeX

@article{3b4e4b3fed894c21aef746231f456002,
title = "Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition",
abstract = "The first results on the interaction between an Fe–Ni melt and anthracene (С14Н10) in the presence of olivine at 3 GPa and 1500°С and on the study of the component composition of the fluid generated in this process are presented. The stability of aliphatic hydrocarbons in the implemented conditions is confirmed experimentally. It is established that, under these conditions, crystallization of high-magnesian olivines occurs (Fo = 97–98 mol %). The composition of the fluid is similar to the composition of the fluid from inclusions in synthetic diamonds. The conditions implemented in the experiment might have occurred at the early stages of the Earth{\textquoteright}s evolution.",
keywords = "diamond, Fe–Ni melt, fluid, high pressures and high temperatures, hydrocarbons, olivine, Fe-Ni melt, POLYCYCLIC AROMATIC-HYDROCARBONS, IRON, DIAMONDS, PLACERS",
author = "Chepurov, {A. I.} and Tomilenko, {A. A.} and Sonin, {V. M.} and Zhimulev, {E. I.} and Bul{\textquoteright}bak, {T. A.} and Chepurov, {A. A.} and Sobolev, {N. V.}",
year = "2020",
month = may,
day = "1",
doi = "10.1134/S1028334X20050050",
language = "English",
volume = "492",
pages = "333--337",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Interaction of an Fe–Ni Melt with Anthracene (C14H10) in the Presence of Olivine at 3 GPa: Fluid Phase Composition

AU - Chepurov, A. I.

AU - Tomilenko, A. A.

AU - Sonin, V. M.

AU - Zhimulev, E. I.

AU - Bul’bak, T. A.

AU - Chepurov, A. A.

AU - Sobolev, N. V.

PY - 2020/5/1

Y1 - 2020/5/1

N2 - The first results on the interaction between an Fe–Ni melt and anthracene (С14Н10) in the presence of olivine at 3 GPa and 1500°С and on the study of the component composition of the fluid generated in this process are presented. The stability of aliphatic hydrocarbons in the implemented conditions is confirmed experimentally. It is established that, under these conditions, crystallization of high-magnesian olivines occurs (Fo = 97–98 mol %). The composition of the fluid is similar to the composition of the fluid from inclusions in synthetic diamonds. The conditions implemented in the experiment might have occurred at the early stages of the Earth’s evolution.

AB - The first results on the interaction between an Fe–Ni melt and anthracene (С14Н10) in the presence of olivine at 3 GPa and 1500°С and on the study of the component composition of the fluid generated in this process are presented. The stability of aliphatic hydrocarbons in the implemented conditions is confirmed experimentally. It is established that, under these conditions, crystallization of high-magnesian olivines occurs (Fo = 97–98 mol %). The composition of the fluid is similar to the composition of the fluid from inclusions in synthetic diamonds. The conditions implemented in the experiment might have occurred at the early stages of the Earth’s evolution.

KW - diamond

KW - Fe–Ni melt

KW - fluid

KW - high pressures and high temperatures

KW - hydrocarbons

KW - olivine

KW - Fe-Ni melt

KW - POLYCYCLIC AROMATIC-HYDROCARBONS

KW - IRON

KW - DIAMONDS

KW - PLACERS

UR - http://www.scopus.com/inward/record.url?scp=85087522854&partnerID=8YFLogxK

U2 - 10.1134/S1028334X20050050

DO - 10.1134/S1028334X20050050

M3 - Article

AN - SCOPUS:85087522854

VL - 492

SP - 333

EP - 337

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 24720300