Arctic Mineral Resources. Science and Technology
The Arctic zone of the Earth is a major source of mineral and other natural resources for the future development of science and technology. It contains a large supply of strategic mineral deposits, including rare earths, copper, phosphorus, niobium, platinum-group elements, and other critical metals...
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| Format: | Book Chapter |
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MDPI - Multidisciplinary Digital Publishing Institute
2019
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| Subjects: | |
| Online Access: | Get Fullteks DOAB: description of the publication |
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| LEADER | 05990naaaa2201573uu 4500 | ||
|---|---|---|---|
| 001 | doab_20_500_12854_41243 | ||
| 005 | 20210211 | ||
| 020 | |a books978-3-03897-825-1 | ||
| 020 | |a 9783038978251 | ||
| 020 | |a 9783038978244 | ||
| 024 | 7 | |a 10.3390/books978-3-03897-825-1 |c doi | |
| 041 | 0 | |a English | |
| 042 | |a dc | ||
| 100 | 1 | |a Krivovichev, Sergey V. |4 auth | |
| 245 | 1 | 0 | |a Arctic Mineral Resources. Science and Technology |
| 260 | |b MDPI - Multidisciplinary Digital Publishing Institute |c 2019 | ||
| 300 | |a 1 electronic resource (432 p.) | ||
| 506 | 0 | |a Open Access |2 star |f Unrestricted online access | |
| 520 | |a The Arctic zone of the Earth is a major source of mineral and other natural resources for the future development of science and technology. It contains a large supply of strategic mineral deposits, including rare earths, copper, phosphorus, niobium, platinum-group elements, and other critical metals. The continued melting of the sea ice due to climate change makes these resources more accessible than ever before. However, the mineral exploration in the Arctic has always been a challenge due to the climatic restrictions, remote location, and vulnerability of Arctic ecosystems. This book covers a broad range of topics related to the problem of Arctic mineral resources, including geological, geochemical, and mineralogical aspects of their occurrence and formation; chemical technologies; and environmental and economic problems related to mineral exploration. The contributions can be tentatively classified into four major types: geodynamics and metallogeny, mineralogy and petrology, mineralogy and crystallography, and mining and chemical technologies associated with the exploration of mineral deposits and the use of raw materials for manufacturing new products. The book can be of interest for all those interested in Arctic issues and especially in Arctic mineral resources and associated problems of mineralogy, geology, geochemistry, and technology. | ||
| 540 | |a Creative Commons |f https://creativecommons.org/licenses/by-nc-nd/4.0/ |2 cc |4 https://creativecommons.org/licenses/by-nc-nd/4.0/ | ||
| 546 | |a English | ||
| 653 | |a U mineralization | ||
| 653 | |a n/a | ||
| 653 | |a ivanyukite | ||
| 653 | |a Kovdor phoscorite-carbonatite complex | ||
| 653 | |a Precambrian | ||
| 653 | |a Kovdor phoscorite-carbonatite complex | ||
| 653 | |a hydrothermal deposits | ||
| 653 | |a chalcopyrite | ||
| 653 | |a cathodoluminescence | ||
| 653 | |a PGE | ||
| 653 | |a low-grade copper-nickel ore | ||
| 653 | |a Northern Karelia | ||
| 653 | |a diamond processing plants | ||
| 653 | |a transformation mineral species | ||
| 653 | |a batievaite-(Y) | ||
| 653 | |a rock alteration | ||
| 653 | |a Khibiny | ||
| 653 | |a bacterial leaching | ||
| 653 | |a cryomineralogenesis | ||
| 653 | |a beryllium minerals | ||
| 653 | |a Siberian craton | ||
| 653 | |a apatite-nepheline deposit | ||
| 653 | |a apatite | ||
| 653 | |a gold | ||
| 653 | |a hainite-(Y) | ||
| 653 | |a Keivy alkaline province | ||
| 653 | |a zircon | ||
| 653 | |a niobium | ||
| 653 | |a zeolite group minerals | ||
| 653 | |a shkatulkalite | ||
| 653 | |a zircon dating | ||
| 653 | |a electrochemical separation | ||
| 653 | |a hydrothermal synthesis | ||
| 653 | |a pyrrhotite | ||
| 653 | |a Breivikbotn | ||
| 653 | |a crystal fractionation | ||
| 653 | |a Sakharjok massif | ||
| 653 | |a Palaeoproterozoic | ||
| 653 | |a titanosilicate | ||
| 653 | |a Pechenga structure | ||
| 653 | |a LIP | ||
| 653 | |a antigorite | ||
| 653 | |a nepheline | ||
| 653 | |a forsterite | ||
| 653 | |a Arctic | ||
| 653 | |a saponite-containing waters | ||
| 653 | |a chemical composition | ||
| 653 | |a Khibiny promising structures | ||
| 653 | |a melteigite | ||
| 653 | |a sulfuric-acidic decomposition | ||
| 653 | |a petroleum potential | ||
| 653 | |a mineralogy | ||
| 653 | |a mafic intrusion | ||
| 653 | |a Paleoproterozoic | ||
| 653 | |a vuonnemite | ||
| 653 | |a calcite | ||
| 653 | |a garnet | ||
| 653 | |a raw materials | ||
| 653 | |a search of trend differences | ||
| 653 | |a metallogeny | ||
| 653 | |a Lovozero alkaline massif | ||
| 653 | |a isotopes | ||
| 653 | |a kimberlite | ||
| 653 | |a phase diagram apatite-nepheline-diopside | ||
| 653 | |a mineral data | ||
| 653 | |a ore dressing tailings | ||
| 653 | |a geochronology | ||
| 653 | |a geodynamic evolution | ||
| 653 | |a pyrochlore supergroup minerals | ||
| 653 | |a pentlandite | ||
| 653 | |a saponite product applications | ||
| 653 | |a basic rocks | ||
| 653 | |a Plume | ||
| 653 | |a West-Pana intrusion | ||
| 653 | |a Rb-Sr | ||
| 653 | |a U-Pb | ||
| 653 | |a heap leaching | ||
| 653 | |a rinkite group minerals | ||
| 653 | |a Arctic zone | ||
| 653 | |a Ti-in-zircon geothermometry | ||
| 653 | |a apatite-nepheline-titanite ore | ||
| 653 | |a cobaltpentlandite | ||
| 653 | |a silicocarbonatite | ||
| 653 | |a Fennoscandian Shield | ||
| 653 | |a titanium | ||
| 653 | |a MHD-source "Khibiny" | ||
| 653 | |a Fedorova-Pana Complex | ||
| 653 | |a Northern Norway | ||
| 653 | |a evolution of the composition | ||
| 653 | |a trace elements | ||
| 653 | |a oil | ||
| 653 | |a vanadium mineralization | ||
| 653 | |a geodynamics | ||
| 653 | |a gas | ||
| 653 | |a greenstone belt | ||
| 653 | |a South Reef | ||
| 653 | |a typochemistry | ||
| 653 | |a mechanical activation | ||
| 653 | |a alkali-activated binder | ||
| 653 | |a Kola region | ||
| 653 | |a hydrothermal veins | ||
| 653 | |a Kola Peninsula | ||
| 653 | |a macrocrysts | ||
| 653 | |a titanyl sulfate | ||
| 653 | |a alkaline rocks | ||
| 653 | |a cryogenic treatment | ||
| 653 | |a granite | ||
| 653 | |a Yenisei-Khatanga basin | ||
| 653 | |a crystal structure | ||
| 653 | |a pegmatites | ||
| 653 | |a conductive layers | ||
| 856 | 4 | 0 | |a www.oapen.org |u https://mdpi.com/books/pdfview/book/1263 |7 0 |z Get Fullteks |
| 856 | 4 | 0 | |a www.oapen.org |u https://directory.doabooks.org/handle/20.500.12854/41243 |7 0 |z DOAB: description of the publication |