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Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters. / Bataleva, Yu V.; Palyanov, Yu N.; Borzdov, Yu M. et al.

In: Doklady Earth Sciences, Vol. 471, No. 1, 01.11.2016, p. 1144-1148.

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

Harvard

Bataleva, YV, Palyanov, YN, Borzdov, YM & Sobolev, NV 2016, 'Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters', Doklady Earth Sciences, vol. 471, no. 1, pp. 1144-1148. https://doi.org/10.1134/S1028334X16110015

APA

Bataleva, Y. V., Palyanov, Y. N., Borzdov, Y. M., & Sobolev, N. V. (2016). Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters. Doklady Earth Sciences, 471(1), 1144-1148. https://doi.org/10.1134/S1028334X16110015

Vancouver

Bataleva YV, Palyanov YN, Borzdov YM, Sobolev NV. Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters. Doklady Earth Sciences. 2016 Nov 1;471(1):1144-1148. doi: 10.1134/S1028334X16110015

Author

Bataleva, Yu V. ; Palyanov, Yu N. ; Borzdov, Yu M. et al. / Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters. In: Doklady Earth Sciences. 2016 ; Vol. 471, No. 1. pp. 1144-1148.

BibTeX

@article{d0a9a53b52604c3ca7bb139d8780a2f3,
title = "Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters",
abstract = "Experimental research in the Fe3C–(Fe,Ni)S system was carried out. The objective of the investigation was to model the reactions of carbide–sulfide interaction related to graphite (diamond) formation in reduced lithosphere mantle domains. T ≤ 1200°C is the formation temperature of the Ni-cohenite + graphite assemblage coexisting with two immiscible melts such as sulfide (Fe60–Ni3–S37)L and metal–sulfide (Fe71–Ni7–S21–C1)L containing dissolved carbon. Т ≥ 1300°C is the generation temperature of a unified melt such as (Fe80–Ni6–S10–C4)L characterized by graphite crystallization and diamond growth. The extraction of carbide carbon during the interaction with the sulfide melt can be considered as one of the potential mechanisms of graphite and diamond formation in the reduced mantle.",
author = "Bataleva, {Yu V.} and Palyanov, {Yu N.} and Borzdov, {Yu M.} and Sobolev, {N. V.}",
year = "2016",
month = nov,
day = "1",
doi = "10.1134/S1028334X16110015",
language = "English",
volume = "471",
pages = "1144--1148",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Graphite and diamond formation via the interaction of iron carbide and Fe,Ni-sulfide under mantle P–T parameters

AU - Bataleva, Yu V.

AU - Palyanov, Yu N.

AU - Borzdov, Yu M.

AU - Sobolev, N. V.

PY - 2016/11/1

Y1 - 2016/11/1

N2 - Experimental research in the Fe3C–(Fe,Ni)S system was carried out. The objective of the investigation was to model the reactions of carbide–sulfide interaction related to graphite (diamond) formation in reduced lithosphere mantle domains. T ≤ 1200°C is the formation temperature of the Ni-cohenite + graphite assemblage coexisting with two immiscible melts such as sulfide (Fe60–Ni3–S37)L and metal–sulfide (Fe71–Ni7–S21–C1)L containing dissolved carbon. Т ≥ 1300°C is the generation temperature of a unified melt such as (Fe80–Ni6–S10–C4)L characterized by graphite crystallization and diamond growth. The extraction of carbide carbon during the interaction with the sulfide melt can be considered as one of the potential mechanisms of graphite and diamond formation in the reduced mantle.

AB - Experimental research in the Fe3C–(Fe,Ni)S system was carried out. The objective of the investigation was to model the reactions of carbide–sulfide interaction related to graphite (diamond) formation in reduced lithosphere mantle domains. T ≤ 1200°C is the formation temperature of the Ni-cohenite + graphite assemblage coexisting with two immiscible melts such as sulfide (Fe60–Ni3–S37)L and metal–sulfide (Fe71–Ni7–S21–C1)L containing dissolved carbon. Т ≥ 1300°C is the generation temperature of a unified melt such as (Fe80–Ni6–S10–C4)L characterized by graphite crystallization and diamond growth. The extraction of carbide carbon during the interaction with the sulfide melt can be considered as one of the potential mechanisms of graphite and diamond formation in the reduced mantle.

UR - http://www.scopus.com/inward/record.url?scp=84999622395&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16110015

DO - 10.1134/S1028334X16110015

M3 - Article

AN - SCOPUS:84999622395

VL - 471

SP - 1144

EP - 1148

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25723658