Standard

Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals). / Stepanov, S. Yu; Sharpenok, L. N.; Antonov, A. V.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 146, № 1, 01.01.2017, стр. 29-43.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Stepanov, SY, Sharpenok, LN & Antonov, AV 2017, 'Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 146, № 1, стр. 29-43.

APA

Stepanov, S. Y., Sharpenok, L. N., & Antonov, A. V. (2017). Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 146(1), 29-43.

Vancouver

Stepanov SY, Sharpenok LN, Antonov AV. Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2017 Янв. 1;146(1):29-43.

Author

Stepanov, S. Yu ; Sharpenok, L. N. ; Antonov, A. V. / Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2017 ; Том 146, № 1. стр. 29-43.

BibTeX

@article{176ef35d2b20404ca6de90971fc367c3,
title = "Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals)",
abstract = "The paper analyses geological position of the Vorontsovskoe gold deposit which is untypical for the Urals folded belt. This deposit is a part of the ore-magmatic system formed in connection with the Auerbakhovsky massif at the North Urals. There are displayed data on mineralogical-geochemical and petrographic characteristics of studied gold-bearing breccias with detail description of their cement. It contains realgar and orpiment, and, in subordinate quantity, Hg-bearing sphalerite, dimorphite, routhierite and minerals of the gruzdevite-aktashite isomorphous series. Obtained data allow to attribute these gold-bearing breccias, with realgar-orpiment cement, to fluid-explosive formations. This is one of numerous evidences to consider ore deposits connected with Auerbakhovsky massif as parts of a uniform ore-magmatic system with distinct lateral zoning.",
keywords = "Auerbakhovsky massif, Copper-porphyry ore system, Fluid-explosive breccias, Orpiment-realgar association, The North Ural, Vorontsovskoe gold-ore deposit",
author = "Stepanov, {S. Yu} and Sharpenok, {L. N.} and Antonov, {A. V.}",
year = "2017",
month = jan,
day = "1",
language = "English",
volume = "146",
pages = "29--43",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "1",

}

RIS

TY - JOUR

T1 - Fluid-explosive breccias of the vorontsovskoe gold deposit (the North Urals)

AU - Stepanov, S. Yu

AU - Sharpenok, L. N.

AU - Antonov, A. V.

PY - 2017/1/1

Y1 - 2017/1/1

N2 - The paper analyses geological position of the Vorontsovskoe gold deposit which is untypical for the Urals folded belt. This deposit is a part of the ore-magmatic system formed in connection with the Auerbakhovsky massif at the North Urals. There are displayed data on mineralogical-geochemical and petrographic characteristics of studied gold-bearing breccias with detail description of their cement. It contains realgar and orpiment, and, in subordinate quantity, Hg-bearing sphalerite, dimorphite, routhierite and minerals of the gruzdevite-aktashite isomorphous series. Obtained data allow to attribute these gold-bearing breccias, with realgar-orpiment cement, to fluid-explosive formations. This is one of numerous evidences to consider ore deposits connected with Auerbakhovsky massif as parts of a uniform ore-magmatic system with distinct lateral zoning.

AB - The paper analyses geological position of the Vorontsovskoe gold deposit which is untypical for the Urals folded belt. This deposit is a part of the ore-magmatic system formed in connection with the Auerbakhovsky massif at the North Urals. There are displayed data on mineralogical-geochemical and petrographic characteristics of studied gold-bearing breccias with detail description of their cement. It contains realgar and orpiment, and, in subordinate quantity, Hg-bearing sphalerite, dimorphite, routhierite and minerals of the gruzdevite-aktashite isomorphous series. Obtained data allow to attribute these gold-bearing breccias, with realgar-orpiment cement, to fluid-explosive formations. This is one of numerous evidences to consider ore deposits connected with Auerbakhovsky massif as parts of a uniform ore-magmatic system with distinct lateral zoning.

KW - Auerbakhovsky massif

KW - Copper-porphyry ore system

KW - Fluid-explosive breccias

KW - Orpiment-realgar association

KW - The North Ural

KW - Vorontsovskoe gold-ore deposit

UR - http://www.scopus.com/inward/record.url?scp=85047923264&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:85047923264

VL - 146

SP - 29

EP - 43

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 1

ER -

ID: 47779201