RASPREDELE. IE Z UPSILON LOTA V INTRUZIVNYKH I POSLEMAGMATICHESKIKH PORODAKH OL'KHOVSKO-CHIBIZHEKSKOGO RUDNOGO POLYA VOSTOCHNOGO SAYANA.

Translated title of the contribution: Gold Distribution in Intrusive Post-Magmatic Rocks of the Ol'khovsk-Chibizheksk Ore Deposit in the East Sayan Area.

A. F. Korobeinikov, A. V. Matsyushevskii, V. L. Chesnokov, E. V. Chernyaev

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Gold behavior is examined in the formation processes of intrusive contact-metasomatic and hydrothermal ore associations of a typical contact-gold ore deposit in the Sayan-Altai folded region. It is shown that crystallization of the magmatic melt of granitoid rocks does not essentially result in gold accumulation although a tendency toward an increased content of this metal is noted in basic rocks and mafic minerals. Partial accumulation of chalcophyles and gold during contact metamorphism has been established. High metal concentration is observed only for the middle-low-temperature hydrothermal stage (320-130 degree C) of general post-magmatic mineral formation.

Original languageRussian
Title of host publicationGeol Geofiz
Pages62-74
Number of pages13
Edition9
Publication statusPublished - Sep 1976

Fingerprint

Ore deposits
Gold
Rocks
Minerals
Metals
Ores
Crystallization
Temperature

ASJC Scopus subject areas

  • Engineering(all)

Cite this

Korobeinikov, A. F., Matsyushevskii, A. V., Chesnokov, V. L., & Chernyaev, E. V. (1976). RASPREDELE. IE Z UPSILON LOTA V INTRUZIVNYKH I POSLEMAGMATICHESKIKH PORODAKH OL'KHOVSKO-CHIBIZHEKSKOGO RUDNOGO POLYA VOSTOCHNOGO SAYANA. In Geol Geofiz (9 ed., pp. 62-74)

RASPREDELE. IE Z UPSILON LOTA V INTRUZIVNYKH I POSLEMAGMATICHESKIKH PORODAKH OL'KHOVSKO-CHIBIZHEKSKOGO RUDNOGO POLYA VOSTOCHNOGO SAYANA. / Korobeinikov, A. F.; Matsyushevskii, A. V.; Chesnokov, V. L.; Chernyaev, E. V.

Geol Geofiz. 9. ed. 1976. p. 62-74.

Research output: Chapter in Book/Report/Conference proceedingChapter

@inbook{24017ed0ea814b209957db492fabc9df,
title = "RASPREDELE. IE Z UPSILON LOTA V INTRUZIVNYKH I POSLEMAGMATICHESKIKH PORODAKH OL'KHOVSKO-CHIBIZHEKSKOGO RUDNOGO POLYA VOSTOCHNOGO SAYANA.",
abstract = "Gold behavior is examined in the formation processes of intrusive contact-metasomatic and hydrothermal ore associations of a typical contact-gold ore deposit in the Sayan-Altai folded region. It is shown that crystallization of the magmatic melt of granitoid rocks does not essentially result in gold accumulation although a tendency toward an increased content of this metal is noted in basic rocks and mafic minerals. Partial accumulation of chalcophyles and gold during contact metamorphism has been established. High metal concentration is observed only for the middle-low-temperature hydrothermal stage (320-130 degree C) of general post-magmatic mineral formation.",
author = "Korobeinikov, {A. F.} and Matsyushevskii, {A. V.} and Chesnokov, {V. L.} and Chernyaev, {E. V.}",
year = "1976",
month = "9",
language = "Русский",
pages = "62--74",
booktitle = "Geol Geofiz",
edition = "9",

}

TY - CHAP

T1 - RASPREDELE. IE Z UPSILON LOTA V INTRUZIVNYKH I POSLEMAGMATICHESKIKH PORODAKH OL'KHOVSKO-CHIBIZHEKSKOGO RUDNOGO POLYA VOSTOCHNOGO SAYANA.

AU - Korobeinikov, A. F.

AU - Matsyushevskii, A. V.

AU - Chesnokov, V. L.

AU - Chernyaev, E. V.

PY - 1976/9

Y1 - 1976/9

N2 - Gold behavior is examined in the formation processes of intrusive contact-metasomatic and hydrothermal ore associations of a typical contact-gold ore deposit in the Sayan-Altai folded region. It is shown that crystallization of the magmatic melt of granitoid rocks does not essentially result in gold accumulation although a tendency toward an increased content of this metal is noted in basic rocks and mafic minerals. Partial accumulation of chalcophyles and gold during contact metamorphism has been established. High metal concentration is observed only for the middle-low-temperature hydrothermal stage (320-130 degree C) of general post-magmatic mineral formation.

AB - Gold behavior is examined in the formation processes of intrusive contact-metasomatic and hydrothermal ore associations of a typical contact-gold ore deposit in the Sayan-Altai folded region. It is shown that crystallization of the magmatic melt of granitoid rocks does not essentially result in gold accumulation although a tendency toward an increased content of this metal is noted in basic rocks and mafic minerals. Partial accumulation of chalcophyles and gold during contact metamorphism has been established. High metal concentration is observed only for the middle-low-temperature hydrothermal stage (320-130 degree C) of general post-magmatic mineral formation.

UR - http://www.scopus.com/inward/record.url?scp=0016998520&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0016998520&partnerID=8YFLogxK

M3 - Глава

SP - 62

EP - 74

BT - Geol Geofiz

ER -