Arctic Mineral Resources. Science and Technology
Krivovichev, Sergey V.
Arctic Mineral Resources. Science and Technology
English[eng]
U mineralization||n/a||ivanyukite||Kovdor phoscorite–carbonatite complex||Precambrian||Kovdor phoscorite-carbonatite complex||hydrothermal deposits||chalcopyrite||cathodoluminescence||PGE||low-grade copper-nickel ore||Northern Karelia||diamond processing plants||transformation mineral species||batievaite-(Y)||rock alteration||Khibiny||bacterial leaching||cryomineralogenesis||beryllium minerals||Siberian craton||apatite-nepheline deposit||apatite||gold||hainite-(Y)||Keivy alkaline province||zircon||niobium||zeolite group minerals||shkatulkalite||zircon dating||electrochemical separation||hydrothermal synthesis||pyrrhotite||Breivikbotn||crystal fractionation||Sakharjok massif||Palaeoproterozoic||titanosilicate||Pechenga structure||LIP||antigorite||nepheline||forsterite||Arctic||saponite-containing waters||chemical composition||Khibiny promising structures||melteigite||sulfuric-acidic decomposition||petroleum potential||mineralogy||mafic intrusion||Paleoproterozoic||vuonnemite||calcite||garnet||raw materials||search of trend differences||metallogeny||Lovozero alkaline massif||isotopes||kimberlite||phase diagram apatite-nepheline-diopside||mineral data||ore dressing tailings||geochronology||geodynamic evolution||pyrochlore supergroup minerals||pentlandite||saponite product applications||basic rocks||Plume||West-Pana intrusion||Rb-Sr||U-Pb||heap leaching||rinkite group minerals||Arctic zone||Ti-in-zircon geothermometry||apatite-nepheline-titanite ore||cobaltpentlandite||silicocarbonatite||Fennoscandian Shield||titanium||MHD-source “Khibinyâ€||Fedorova-Pana Complex||Northern Norway||evolution of the composition||trace elements||oil||vanadium mineralization||geodynamics||gas||greenstone belt||South Reef||typochemistry||mechanical activation||alkali-activated binder||Kola region||hydrothermal veins||Kola Peninsula||macrocrysts||titanyl sulfate||alkaline rocks||cryogenic treatment||granite||Yenisei-Khatanga basin||crystal structure||pegmatites||conductive layers
Arctic Mineral Resources. Science and Technology
English[eng]
U mineralization||n/a||ivanyukite||Kovdor phoscorite–carbonatite complex||Precambrian||Kovdor phoscorite-carbonatite complex||hydrothermal deposits||chalcopyrite||cathodoluminescence||PGE||low-grade copper-nickel ore||Northern Karelia||diamond processing plants||transformation mineral species||batievaite-(Y)||rock alteration||Khibiny||bacterial leaching||cryomineralogenesis||beryllium minerals||Siberian craton||apatite-nepheline deposit||apatite||gold||hainite-(Y)||Keivy alkaline province||zircon||niobium||zeolite group minerals||shkatulkalite||zircon dating||electrochemical separation||hydrothermal synthesis||pyrrhotite||Breivikbotn||crystal fractionation||Sakharjok massif||Palaeoproterozoic||titanosilicate||Pechenga structure||LIP||antigorite||nepheline||forsterite||Arctic||saponite-containing waters||chemical composition||Khibiny promising structures||melteigite||sulfuric-acidic decomposition||petroleum potential||mineralogy||mafic intrusion||Paleoproterozoic||vuonnemite||calcite||garnet||raw materials||search of trend differences||metallogeny||Lovozero alkaline massif||isotopes||kimberlite||phase diagram apatite-nepheline-diopside||mineral data||ore dressing tailings||geochronology||geodynamic evolution||pyrochlore supergroup minerals||pentlandite||saponite product applications||basic rocks||Plume||West-Pana intrusion||Rb-Sr||U-Pb||heap leaching||rinkite group minerals||Arctic zone||Ti-in-zircon geothermometry||apatite-nepheline-titanite ore||cobaltpentlandite||silicocarbonatite||Fennoscandian Shield||titanium||MHD-source “Khibinyâ€||Fedorova-Pana Complex||Northern Norway||evolution of the composition||trace elements||oil||vanadium mineralization||geodynamics||gas||greenstone belt||South Reef||typochemistry||mechanical activation||alkali-activated binder||Kola region||hydrothermal veins||Kola Peninsula||macrocrysts||titanyl sulfate||alkaline rocks||cryogenic treatment||granite||Yenisei-Khatanga basin||crystal structure||pegmatites||conductive layers