PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)

Fluid inclusions are studied in calcite from magnetite ores and sulfide-carbonate veins of the Aktash sulfide-magnetite deposit (Western Karanazar, Tajikistan) to identify their formation conditions. The deposit is confined to a contact zone between carbonate (Upper Devonian–Lower Carboniferous dolo...

Full description

Saved in:
Bibliographic Details
Main Authors: U.A. Yatimov, N.N. Ankusheva, M.A. Rassomakhin
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2021-12-01
Series:Минералогия
Subjects:
Online Access:https://journal.mineralogy.ru/wp-content/uploads/2021/12/2021_7_4_4.pdf
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1823856528330850304
author U.A. Yatimov
N.N. Ankusheva
M.A. Rassomakhin
author_facet U.A. Yatimov
N.N. Ankusheva
M.A. Rassomakhin
author_sort U.A. Yatimov
collection DOAJ
description Fluid inclusions are studied in calcite from magnetite ores and sulfide-carbonate veins of the Aktash sulfide-magnetite deposit (Western Karanazar, Tajikistan) to identify their formation conditions. The deposit is confined to a contact zone between carbonate (Upper Devonian–Lower Carboniferous dolomite and limestones) and intrusive rocks (Middle Carboniferous–Early Triassic granodiorites and porphyry granodiorites) of the Kansai ore field. The fluid inclusion study showed that calcite of ore veins formed from moderately saline (4.4–10.8 wt. % NaCl-equiv.) aqueous Na-K ± Mg chloride fluids at a decreasing temperature from 300 to 160 °C. The homogenization temperatures of fluid inclusions are consistent with thermometric data for chlorite, which formed together with calcite (176–295 °C).
format Article
id doaj-art-bce9355beddc401695e3d6698fcbd340
institution Kabale University
issn 2313-545X
2782-2044
language English
publishDate 2021-12-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
record_format Article
series Минералогия
spelling doaj-art-bce9355beddc401695e3d6698fcbd3402025-02-12T08:21:49ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442021-12-0174627110.35597/2313-545X-2021-7-4-4PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)U.A. Yatimov0N.N. Ankusheva1M.A. Rassomakhin2South Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASFluid inclusions are studied in calcite from magnetite ores and sulfide-carbonate veins of the Aktash sulfide-magnetite deposit (Western Karanazar, Tajikistan) to identify their formation conditions. The deposit is confined to a contact zone between carbonate (Upper Devonian–Lower Carboniferous dolomite and limestones) and intrusive rocks (Middle Carboniferous–Early Triassic granodiorites and porphyry granodiorites) of the Kansai ore field. The fluid inclusion study showed that calcite of ore veins formed from moderately saline (4.4–10.8 wt. % NaCl-equiv.) aqueous Na-K ± Mg chloride fluids at a decreasing temperature from 300 to 160 °C. The homogenization temperatures of fluid inclusions are consistent with thermometric data for chlorite, which formed together with calcite (176–295 °C).https://journal.mineralogy.ru/wp-content/uploads/2021/12/2021_7_4_4.pdfcalcitechloriteformation conditionsfluid inclusionspolymetallic oresmagnetite oresaktash depositwestern karamazar
spellingShingle U.A. Yatimov
N.N. Ankusheva
M.A. Rassomakhin
PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
Минералогия
calcite
chlorite
formation conditions
fluid inclusions
polymetallic ores
magnetite ores
aktash deposit
western karamazar
title PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
title_full PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
title_fullStr PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
title_full_unstemmed PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
title_short PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN)
title_sort pt formation conditions of polymetallic ores from the pb zn fe aktash skarn deposit western karamazar tajikistan
topic calcite
chlorite
formation conditions
fluid inclusions
polymetallic ores
magnetite ores
aktash deposit
western karamazar
url https://journal.mineralogy.ru/wp-content/uploads/2021/12/2021_7_4_4.pdf
work_keys_str_mv AT uayatimov ptformationconditionsofpolymetallicoresfromthepbznfeaktashskarndepositwesternkaramazartajikistan
AT nnankusheva ptformationconditionsofpolymetallicoresfromthepbznfeaktashskarndepositwesternkaramazartajikistan
AT marassomakhin ptformationconditionsofpolymetallicoresfromthepbznfeaktashskarndepositwesternkaramazartajikistan