TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA

The aim of the study is the determination of mineralogical and geochemical features of magnetite from massive sulfide and iron deposits to develop forecasting criteria of ore objects. The layered magnetitolites of sulfide (Mauk, Letnee, Sibai and Molodezhnoe) and stratiform iron (Kachar, Sarbai,...

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Main Authors: V.V. Maslennikov, N.R. Ayupova, A.S. Tseluyko, N.P. Safina, D.A. Artemyev, U.A. Yatimov, S.I. Bryukhov, P.V. Khvorov, M.A. Rassomakhin
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2025-12-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_1.pdf
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author V.V. Maslennikov
N.R. Ayupova
A.S. Tseluyko
N.P. Safina
D.A. Artemyev
U.A. Yatimov
S.I. Bryukhov
P.V. Khvorov
M.A. Rassomakhin
author_facet V.V. Maslennikov
N.R. Ayupova
A.S. Tseluyko
N.P. Safina
D.A. Artemyev
U.A. Yatimov
S.I. Bryukhov
P.V. Khvorov
M.A. Rassomakhin
author_sort V.V. Maslennikov
collection DOAJ
description The aim of the study is the determination of mineralogical and geochemical features of magnetite from massive sulfide and iron deposits to develop forecasting criteria of ore objects. The layered magnetitolites of sulfide (Mauk, Letnee, Sibai and Molodezhnoe) and stratiform iron (Kachar, Sarbai, Estyuninskoe, Osokino-Aleksandrovskoe and Techa) deposits of volcanosedimentary association are the objects of study. It is established using laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) that, in contrast to magnetite of iron deposits, magnetite of ore-controlling volcanosedimentary horizons of the Urals massive sulfide deposits is characterized by a higher content and stable associations of Bi, Te, Co, As, Cd, Zn, Cu and Mo due to relict inclusions of sulfide clasts and products of their halmyrolysis. The elevated Ti, V and Zr contents, as well as the mixed associations of lithophile, siderophile and chalcophile elements, are more typical of magnetite of iron deposits after hyaloclastites. Typochemistry of magnetite from volcanosedimentary horizons can be a criterion for searching the massive sulfide deposits
format Article
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institution Kabale University
issn 2313-545X
2782-2044
language English
publishDate 2025-12-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
record_format Article
series Минералогия
spelling doaj-art-5d623608502f4559877d7a4c8321bbab2025-02-06T10:17:33ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442025-12-0110484010.35597/2313-545X-2024-10-4-1TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATAV.V. Maslennikov0https://orcid.org/0000-0002-1999-2324N.R. Ayupova1A.S. Tseluyko2N.P. Safina3D.A. Artemyev4U.A. Yatimov5S.I. Bryukhov6P.V. Khvorov7M.A. Rassomakhin8South 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 RASSouth 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 RASSouth 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 RASThe aim of the study is the determination of mineralogical and geochemical features of magnetite from massive sulfide and iron deposits to develop forecasting criteria of ore objects. The layered magnetitolites of sulfide (Mauk, Letnee, Sibai and Molodezhnoe) and stratiform iron (Kachar, Sarbai, Estyuninskoe, Osokino-Aleksandrovskoe and Techa) deposits of volcanosedimentary association are the objects of study. It is established using laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) that, in contrast to magnetite of iron deposits, magnetite of ore-controlling volcanosedimentary horizons of the Urals massive sulfide deposits is characterized by a higher content and stable associations of Bi, Te, Co, As, Cd, Zn, Cu and Mo due to relict inclusions of sulfide clasts and products of their halmyrolysis. The elevated Ti, V and Zr contents, as well as the mixed associations of lithophile, siderophile and chalcophile elements, are more typical of magnetite of iron deposits after hyaloclastites. Typochemistry of magnetite from volcanosedimentary horizons can be a criterion for searching the massive sulfide depositshttps://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_1.pdfmagnetitetrace elementsmassive sulfide depositsiron depositsurals
spellingShingle V.V. Maslennikov
N.R. Ayupova
A.S. Tseluyko
N.P. Safina
D.A. Artemyev
U.A. Yatimov
S.I. Bryukhov
P.V. Khvorov
M.A. Rassomakhin
TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
Минералогия
magnetite
trace elements
massive sulfide deposits
iron deposits
urals
title TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
title_full TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
title_fullStr TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
title_full_unstemmed TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
title_short TYPOCHEMISTRY OF MAGNETITE FROM MASSIVE SULFIDE AND IRON DEPOSITS OF THE URALS ACCORDING TO LA-ISP-MS DATA
title_sort typochemistry of magnetite from massive sulfide and iron deposits of the urals according to la isp ms data
topic magnetite
trace elements
massive sulfide deposits
iron deposits
urals
url https://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_1.pdf
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