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Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia). / Kiseleva, Ol'Ga; Airiyants, Evgeniya; Belyanin, Dmytriy et al.

In: E3S Web of Conferences, Vol. 98, 08014, 07.06.2019.

Research output: Contribution to journal › Conference article › peer-review

Harvard

Kiseleva, OG, Airiyants, E, Belyanin, D & Zhmodik, S 2019, 'Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia)', E3S Web of Conferences, vol. 98, 08014. https://doi.org/10.1051/e3sconf/20199808014

APA

Kiseleva, OG., Airiyants, E., Belyanin, D., & Zhmodik, S. (2019). Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia). E3S Web of Conferences, 98, [08014]. https://doi.org/10.1051/e3sconf/20199808014

Vancouver

Kiseleva OG, Airiyants E, Belyanin D, Zhmodik S. Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia). E3S Web of Conferences. 2019 Jun 7;98:08014. doi: 10.1051/e3sconf/20199808014

Author

Kiseleva, Ol'Ga ; Airiyants, Evgeniya ; Belyanin, Dmytriy et al. / Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia). In: E3S Web of Conferences. 2019 ; Vol. 98.

BibTeX

@article{891ec9e8b48e4a1e94da453193ac0cc9,
title = "Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia)",
abstract = "Serpentinization is an important post-magmatic process in spreading and subducted zones. This process is the cause of the remobilization and redistribution of highly mobile elements, platinum group elements (PGE) and base metals. Secondary platinum group minerals (PGMs) formed because of PGE remobilization under the action of mantle and crustal fluid on the rocks. The formation of the secondary PGMs can occur in several stages. Under the effect on the chromitites of reduced mantle fluids, native PGE alloys were formed during early serpentinization. Under dehydrating subducted slab fluid phase was caused in serpentinization mantle peridotites and have been dissolved magmatic high-temperature platinum group minerals. During the obduction of ophiolites, an inversion from reducing to oxidizing condition took place with the formation of nickel arsenides and As, Sb - bearing PGMs.",
keywords = "PGE MINERALIZATION, COMPLEX, ALLOYS, IR, OS",
author = "Ol'Ga Kiseleva and Evgeniya Airiyants and Dmytriy Belyanin and Sergey Zhmodik",
year = "2019",
month = jun,
day = "7",
doi = "10.1051/e3sconf/20199808014",
language = "English",
volume = "98",
journal = "E3S Web of Conferences",
issn = "2555-0403",
publisher = "EDP Sciences",
note = "16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference ; Conference date: 21-07-2019 Through 26-07-2019",

}

RIS

TY - JOUR

T1 - Hydrothermal remobilization platinum group elements and their secondary minerals in chromitite deposits of the Eastern Sayan ophiolites (Russia)

AU - Kiseleva, Ol'Ga

AU - Airiyants, Evgeniya

AU - Belyanin, Dmytriy

AU - Zhmodik, Sergey

PY - 2019/6/7

Y1 - 2019/6/7

N2 - Serpentinization is an important post-magmatic process in spreading and subducted zones. This process is the cause of the remobilization and redistribution of highly mobile elements, platinum group elements (PGE) and base metals. Secondary platinum group minerals (PGMs) formed because of PGE remobilization under the action of mantle and crustal fluid on the rocks. The formation of the secondary PGMs can occur in several stages. Under the effect on the chromitites of reduced mantle fluids, native PGE alloys were formed during early serpentinization. Under dehydrating subducted slab fluid phase was caused in serpentinization mantle peridotites and have been dissolved magmatic high-temperature platinum group minerals. During the obduction of ophiolites, an inversion from reducing to oxidizing condition took place with the formation of nickel arsenides and As, Sb - bearing PGMs.

AB - Serpentinization is an important post-magmatic process in spreading and subducted zones. This process is the cause of the remobilization and redistribution of highly mobile elements, platinum group elements (PGE) and base metals. Secondary platinum group minerals (PGMs) formed because of PGE remobilization under the action of mantle and crustal fluid on the rocks. The formation of the secondary PGMs can occur in several stages. Under the effect on the chromitites of reduced mantle fluids, native PGE alloys were formed during early serpentinization. Under dehydrating subducted slab fluid phase was caused in serpentinization mantle peridotites and have been dissolved magmatic high-temperature platinum group minerals. During the obduction of ophiolites, an inversion from reducing to oxidizing condition took place with the formation of nickel arsenides and As, Sb - bearing PGMs.

KW - PGE MINERALIZATION

KW - COMPLEX

KW - ALLOYS

KW - IR

KW - OS

UR - http://www.scopus.com/inward/record.url?scp=85067305050&partnerID=8YFLogxK

U2 - 10.1051/e3sconf/20199808014

DO - 10.1051/e3sconf/20199808014

M3 - Conference article

AN - SCOPUS:85067305050

VL - 98

JO - E3S Web of Conferences

JF - E3S Web of Conferences

SN - 2555-0403

M1 - 08014

T2 - 16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference

Y2 - 21 July 2019 through 26 July 2019

ER -

ID: 20585200