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This study presents the first fluid inclusion data from quartz of albite–carbonate–quartz altered rocks and metasomatic quartzite hosting gold mineralization in the Pechenga structure of the Pechenga– Imandra–Varzuga greenstone belt. A temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::176993c4ad9a4db21494da24df68ab12
Autor:
Prokofiev VY; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, Moscow, 119117, Russia. vpr2004@rambler.ru., Banks DA; School of Earth and Environment, University of Leeds, Leeds, UK., Lobanov KV; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, Moscow, 119117, Russia., Selektor SL; A.N. Frumkin Institute of Physical Chemistry and Electrochemistry RAS, Moscow, 119071, Russia., Milichko VA; Faculty of Physics and Engineering, ITMO University, St. Petersburg, 197101, Russia., Akinfiev NN; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, Moscow, 119117, Russia., Borovikov AA; Sobolev V.S. Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia., Lüders V; GFZ German Research Centre for Geosciences, Telegrafenberg, 14473, Potsdam, Germany., Chicherov MV; Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, Moscow, 119117, Russia.
Publikováno v:
Scientific reports [Sci Rep] 2020 Jan 24; Vol. 10 (1), pp. 1108. Date of Electronic Publication: 2020 Jan 24.
