Chrome spinels and accessory mineralization in the weathering crust of the Vladimir deposit, Varshavsky ultramafic massif, southern Urals
The paper presents the characteristics of chrome spinels from an ore-bearing packet of the Vladimir chromite deposit. Three main types of chrome spinels are distinguished by morphology and chemical composition: medium-chrome ore-forming, high-chrome transformed, and low-chrome relict accessory. The...
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Veröffentlicht in: | Geology of ore deposits 2016-12, Vol.58 (8), p.697-710 |
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description | The paper presents the characteristics of chrome spinels from an ore-bearing packet of the Vladimir chromite deposit. Three main types of chrome spinels are distinguished by morphology and chemical composition: medium-chrome ore-forming, high-chrome transformed, and low-chrome relict accessory. The significant role of weathering conditions is expressed in alteration of accessory chrome spinel. The formation of high-chrome spinels is explained by the hydrothermal effect of the Varshavsky granitoid massif with accompanying dikes and talc–carbonate metasomatic rocks. Characteristic accessory minerals are represented by native gold and nickel, millerite, pentlandite, chalcopyrite, maucherite, PGE sulfides, and picroilmenite. |
doi_str_mv | 10.1134/S1075701516080031 |
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Characteristic accessory minerals are represented by native gold and nickel, millerite, pentlandite, chalcopyrite, maucherite, PGE sulfides, and picroilmenite.</description><identifier>ISSN: 1075-7015</identifier><identifier>EISSN: 1555-6476</identifier><identifier>DOI: 10.1134/S1075701516080031</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Carbonates ; Chalcopyrite ; Chemical composition ; Chromite ; Dikes ; Earth and Environmental Science ; Earth Sciences ; Embankments ; Gold ; Mineral Resources ; Mineralization ; Minerals and Mineral Assemblages ; Morphology ; Nickel ; Nickel ores ; Organic chemistry ; Pentlandite ; Spinel ; Talc ; Weathering</subject><ispartof>Geology of ore deposits, 2016-12, Vol.58 (8), p.697-710</ispartof><rights>Pleiades Publishing, Ltd. 2016</rights><rights>Copyright Springer Science & Business Media 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-176651909758f220ac394bb072ef39508d0507bee342f7c8daa892dcd8861c653</citedby><cites>FETCH-LOGICAL-a339t-176651909758f220ac394bb072ef39508d0507bee342f7c8daa892dcd8861c653</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1075701516080031$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1075701516080031$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Ankushev, M. 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Characteristic accessory minerals are represented by native gold and nickel, millerite, pentlandite, chalcopyrite, maucherite, PGE sulfides, and picroilmenite.</description><subject>Carbonates</subject><subject>Chalcopyrite</subject><subject>Chemical composition</subject><subject>Chromite</subject><subject>Dikes</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Embankments</subject><subject>Gold</subject><subject>Mineral Resources</subject><subject>Mineralization</subject><subject>Minerals and Mineral Assemblages</subject><subject>Morphology</subject><subject>Nickel</subject><subject>Nickel ores</subject><subject>Organic chemistry</subject><subject>Pentlandite</subject><subject>Spinel</subject><subject>Talc</subject><subject>Weathering</subject><issn>1075-7015</issn><issn>1555-6476</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp1UMtKxDAUDaLgOPoB7gJup3qTNk26lMEXCC50ZlsyaepkbJua2yrjH_jXto4LQVydyz0vOIScMjhnLE4uHhlIIYEJloICiNkemTAhRJQmMt0f7oGORv6QHCFuABLBgU3I53wdfG0ptq6xFVLdFFQbYxF92NJ6eAZduQ_dOd9Q19Bubem71QME1zxTE3rsqC-__8tKF652gRa29ei6GV3qgGv9hi9b2ldd0LUunaG1RnTljKLvx5yGLoYOPCYH5QD25AenZHF99TS_je4fbu7ml_eRjuOsi5hMU8EyyKRQJeegTZwlqxVIbss4E6AKECBX1sYJL6VRhdYq44UplEqZSUU8JWe73Db4195il298H5qhMmdKgUwzzkcV26lM8IjBlnkbXK3DNmeQj4vnfxYfPHznwXYcx4Zfyf-avgBNCoRK</recordid><startdate>20161201</startdate><enddate>20161201</enddate><creator>Ankushev, M. 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subjects | Carbonates Chalcopyrite Chemical composition Chromite Dikes Earth and Environmental Science Earth Sciences Embankments Gold Mineral Resources Mineralization Minerals and Mineral Assemblages Morphology Nickel Nickel ores Organic chemistry Pentlandite Spinel Talc Weathering |
title | Chrome spinels and accessory mineralization in the weathering crust of the Vladimir deposit, Varshavsky ultramafic massif, southern Urals |
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