Standard

Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits). / Kalinin, Yu A.; Palyanova, G. A.; Bortnikov, N. S. et al.

In: Doklady Earth Sciences, Vol. 482, No. 1, 01.09.2018, p. 1193-1198.

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

Harvard

Kalinin, YA, Palyanova, GA, Bortnikov, NS, Naumov, EA & Kovalev, KR 2018, 'Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits)', Doklady Earth Sciences, vol. 482, no. 1, pp. 1193-1198. https://doi.org/10.1134/S1028334X18090131

APA

Kalinin, Y. A., Palyanova, G. A., Bortnikov, N. S., Naumov, E. A., & Kovalev, K. R. (2018). Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits). Doklady Earth Sciences, 482(1), 1193-1198. https://doi.org/10.1134/S1028334X18090131

Vancouver

Kalinin YA, Palyanova GA, Bortnikov NS, Naumov EA, Kovalev KR. Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits). Doklady Earth Sciences. 2018 Sept 1;482(1):1193-1198. doi: 10.1134/S1028334X18090131

Author

Kalinin, Yu A. ; Palyanova, G. A. ; Bortnikov, N. S. et al. / Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits). In: Doklady Earth Sciences. 2018 ; Vol. 482, No. 1. pp. 1193-1198.

BibTeX

@article{d77f4aaa463241c4a80a0325adeef666,
title = "Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits)",
abstract = "The supergene Au in weathering crusts of both the Suzdal and Raygorodok deposits is characterized by enhanced fineness, grain size, crystallinity, and the appearance of botryoidal aggregates of crystals. In the weathering crust of the Suzdal deposit, the exogenous Au is associated primarily with scorodite and carbonates; for Raygorodok, with chalcocite, bornite, hydrocarbonates and Cu hydrosulfates. The difference in the mineral associations of supergene Au at the deposits is determined by the occurrence of various mineral concentrators of Au in the primary endogenous substrate: arsenopyrite and pyrite at the Suzdal deposit and chalcopyrite with pyrite at the Raygorodok deposit. Due to the much greater mobility of Ag in the supergene zone, the weathering crusts are likely to contain submicron microinclusions of Ag minerals beyond the zones of Au concentration.",
author = "Kalinin, {Yu A.} and Palyanova, {G. A.} and Bortnikov, {N. S.} and Naumov, {E. A.} and Kovalev, {K. R.}",
year = "2018",
month = sep,
day = "1",
doi = "10.1134/S1028334X18090131",
language = "English",
volume = "482",
pages = "1193--1198",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Aggregation and Differentiation of Gold and Silver during the Formation of the Gold-Bearing Weathering Crusts (on the Example of Kazakhstan Deposits)

AU - Kalinin, Yu A.

AU - Palyanova, G. A.

AU - Bortnikov, N. S.

AU - Naumov, E. A.

AU - Kovalev, K. R.

PY - 2018/9/1

Y1 - 2018/9/1

N2 - The supergene Au in weathering crusts of both the Suzdal and Raygorodok deposits is characterized by enhanced fineness, grain size, crystallinity, and the appearance of botryoidal aggregates of crystals. In the weathering crust of the Suzdal deposit, the exogenous Au is associated primarily with scorodite and carbonates; for Raygorodok, with chalcocite, bornite, hydrocarbonates and Cu hydrosulfates. The difference in the mineral associations of supergene Au at the deposits is determined by the occurrence of various mineral concentrators of Au in the primary endogenous substrate: arsenopyrite and pyrite at the Suzdal deposit and chalcopyrite with pyrite at the Raygorodok deposit. Due to the much greater mobility of Ag in the supergene zone, the weathering crusts are likely to contain submicron microinclusions of Ag minerals beyond the zones of Au concentration.

AB - The supergene Au in weathering crusts of both the Suzdal and Raygorodok deposits is characterized by enhanced fineness, grain size, crystallinity, and the appearance of botryoidal aggregates of crystals. In the weathering crust of the Suzdal deposit, the exogenous Au is associated primarily with scorodite and carbonates; for Raygorodok, with chalcocite, bornite, hydrocarbonates and Cu hydrosulfates. The difference in the mineral associations of supergene Au at the deposits is determined by the occurrence of various mineral concentrators of Au in the primary endogenous substrate: arsenopyrite and pyrite at the Suzdal deposit and chalcopyrite with pyrite at the Raygorodok deposit. Due to the much greater mobility of Ag in the supergene zone, the weathering crusts are likely to contain submicron microinclusions of Ag minerals beyond the zones of Au concentration.

UR - http://www.scopus.com/inward/record.url?scp=85054823112&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18090131

DO - 10.1134/S1028334X18090131

M3 - Article

AN - SCOPUS:85054823112

VL - 482

SP - 1193

EP - 1198

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25490202