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| 02864cam 2200469zi 4500 |
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| 001 | 9.931060 |
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| 003 | CaOODSP |
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| 005 | 20240112142607 |
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| 006 | m o d f |
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| 007 | cr mn||||||||| |
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| 008 | 231201t20242024onca ob f000 0 eng d |
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| 020 | |a9780660691411 |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 086 | 1 |aM41-11/167-2024E-PDF |
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| 100 | 1 |aCawood, T. K., |eauthor. |
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| 245 | 14|aThe geology of critical battery metals : |ba spotlight on Co in VMS deposits and Li in pegmatites / |cT.K. Cawood and J.M. Peter. |
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| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2024. |
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| 264 | 4|c©2024 |
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| 300 | |a1 online resource (2 pages, 31 unnumbered pages) : |billustrations (chiefly colour). |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aScientific presentation ; |v167 |
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| 500 | |a"Presented at: Central Canada Mineral Exploration Convention. Date presented: 6 November 2023"--Page 2. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"As we move away from a fossil fuel-driven economy, the demand for metals used in energy-dense, rechargeable batteries is increasing; these include cobalt and lithium. Although cobalt is mostly obtained as a by-product from nickel and copper mining, significant amounts also occur in volcanogenic massive sulfide (VMS) deposits, of which Canada has many. However, the primary controls on cobalt distribution in VMS deposits are poorly understood, and may be affected by deformation and metamorphism. We show that cobalt can occur in pyrite, which retains its primary composition through greenschist facies metamorphism; and in pyrrhotite, which expels some cobalt during deformation to form cobaltite crystals. In contrast, most of the global lithium supply is derived from rare metal pegmatites and salars, with pegmatites the most important Canadian source. Our preliminary results confirm that lithium-bearing pegmatites can form directly during anatexis, as well as from fractional crystallization of large bodies of granitic magma"--Abstract (provided by publisher). |
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| 650 | 0|aCobalt. |
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| 650 | 0|aSulfide minerals. |
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| 650 | 0|aOre deposits. |
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| 650 | 0|aLithium. |
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| 650 | 0|aPegmatites. |
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| 650 | 0|aLithium ion batteries|xMaterials. |
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| 650 | 6|aCobalt. |
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| 650 | 6|aSulfures (Minéralogie) |
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| 650 | 6|aGîtes minéraux. |
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| 650 | 6|aLithium. |
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| 650 | 6|aPegmatites. |
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| 650 | 6|aBatteries au lithium-ion|xMatériaux. |
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| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
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| 830 | #0|aScientific presentation (Geological Survey of Canada)|v167.|w(CaOODSP)9.820265 |
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| 856 | 40|qPDF|s42.05 MB|uhttps://publications.gc.ca/collections/collection_2024/rncan-nrcan/m41-11/M41-11-167-2024-eng.pdf |
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| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/332348 |
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