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      <marc:subfield code="a">Cawood, T. K., </marc:subfield>
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      <marc:subfield code="a">The geology of critical battery metals : </marc:subfield>
      <marc:subfield code="b">a spotlight on Co in VMS deposits and Li in pegmatites / </marc:subfield>
      <marc:subfield code="c">T.K. Cawood and J.M. Peter.</marc:subfield>
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      <marc:subfield code="a">[Ottawa] : </marc:subfield>
      <marc:subfield code="b">Geological Survey of Canada, </marc:subfield>
      <marc:subfield code="c">2024.</marc:subfield>
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      <marc:subfield code="c">©2024</marc:subfield>
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      <marc:subfield code="a">1 online resource (2 pages, 31 unnumbered pages) : </marc:subfield>
      <marc:subfield code="b">illustrations (chiefly colour).</marc:subfield>
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      <marc:subfield code="a">Scientific presentation ; </marc:subfield>
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      <marc:subfield code="a">"Presented at: Central Canada Mineral Exploration Convention. Date presented: 6 November 2023"--Page 2.</marc:subfield>
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      <marc:subfield code="a">Includes bibliographical references.</marc:subfield>
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      <marc:subfield code="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).</marc:subfield>
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      <marc:subfield code="a">Cobalt.</marc:subfield>
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      <marc:subfield code="a">Sulfide minerals.</marc:subfield>
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      <marc:subfield code="a">Ore deposits.</marc:subfield>
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      <marc:subfield code="a">Lithium.</marc:subfield>
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      <marc:subfield code="a">Pegmatites.</marc:subfield>
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      <marc:subfield code="a">Lithium ion batteries</marc:subfield>
      <marc:subfield code="x">Materials.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="6">
      <marc:subfield code="a">Cobalt.</marc:subfield>
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      <marc:subfield code="a">Sulfures (Minéralogie)</marc:subfield>
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      <marc:subfield code="a">Lithium.</marc:subfield>
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      <marc:subfield code="a">Pegmatites.</marc:subfield>
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      <marc:subfield code="a">Batteries au lithium-ion</marc:subfield>
      <marc:subfield code="x">Matériaux.</marc:subfield>
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      <marc:subfield code="a">Geological Survey of Canada, </marc:subfield>
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      <marc:subfield code="a">Scientific presentation (Geological Survey of Canada)</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">42.05 MB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2024/rncan-nrcan/m41-11/M41-11-167-2024-eng.pdf</marc:subfield>
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      <marc:subfield code="u">https://doi.org/10.4095/332348</marc:subfield>
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