Articles | Volume 33, issue 4
https://doi.org/10.5194/ejm-33-433-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-33-433-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ardennite-bearing mineral association related to sulfide-free ores with chalcophile metals at Nežilovo, Pelagonian Massif, North Macedonia
Faculty of Science, University of Zagreb, HR – 10000 Zagreb,
Republic of Croatia
Nikita V. Chukanov
Institute of Problems of Chemical Physics, Russian Academy of
Sciences, Chernogolovka, Moscow region, 142432, Russia
Ivan Boev
Faculty of Natural and Technical Sciences, Goce Delčev University, Štip, 2000, Republic of North
Macedonia
Božidar Darko Šturman
Department of Mineralogy and Geology, Royal Ontario Museum, 100 Queen's Park, Toronto, Ontario, Canada
deceased
Vladimir Zebec
Natural History Museum, Demetrova 1, HR – 10000 Zagreb, Republic of Croatia
Vladimir Bermanec
Faculty of Metallurgy, University of Zagreb, Aleja narodnih heroja 3, HR – 44000 Sisak,
Republic of Croatia
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We investigate how trace elements are incorporated into quartz formed in magmatic–hydrothermal ore deposits, key environments for critical metal enrichment. By tracking Li, B, Al, Ti, and OH defects across crystal growth zones we reveal distinct trace element zonation patterns linked to temperature and pressure evolution during crystallization. We demonstrate that combined trace element data and mapping of quartz can be a powerful tool for understanding ore deposit genesis and prospecting ores.
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We investigate how trace elements are incorporated into quartz formed in magmatic–hydrothermal ore deposits, key environments for critical metal enrichment. By tracking Li, B, Al, Ti, and OH defects across crystal growth zones we reveal distinct trace element zonation patterns linked to temperature and pressure evolution during crystallization. We demonstrate that combined trace element data and mapping of quartz can be a powerful tool for understanding ore deposit genesis and prospecting ores.
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The nolanite supergroup has been established and approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association. It contains eight mineral species with the nolanite-type structure. The nolanite supergroup is subdivided into three groups (nolanite, kamiokite, and rinmanite groups). After significant changes, the classification of the nolanite supergroup was approved again.
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The study of the original material of beraunite from the type locality Hrbek, Czech Rep., from collections of the TU Bergakademie Freiberg (Germany) and National Museum Prague (Czech Republic) proved the identity of the minerals beraunite and eleonorite. Because the name beraunite has priority, we consider the name eleonorite to be redundant and proposed to abolish it. The proposal 21-D approved by the IMA discredited eleonorite and accepted the formula of beraunite Fe3+6(PO4)4O(OH)4·6H2O.
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Short summary
A new locality of ardennite-(As) is described in Nežilovo, North Macedonia. This mineral grows in specific conditions, which makes it useful to reconstructing the conditions of rock formation. Phengite mica that was found also supports this investigation. This explanation results in a new proposal for mineral formula calculation of ardennite-group minerals and reviews the current ardennite-group end-members. This occurrence has developed through three metamorphic stages which are also described.
A new locality of ardennite-(As) is described in Nežilovo, North Macedonia. This mineral grows...