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      <marc:subfield code="a">Hayward, N. </marc:subfield>
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    <marc:datafield tag="245" ind1="1" ind2="2">
      <marc:subfield code="a">A comparison of 3-D inversion strategies in the investigation of the 3-D density and magnetic susceptibility distribution in the Great Bear magmatic zone, Northwest Territories / </marc:subfield>
      <marc:subfield code="c">N. Hayward and V. Tschirhart.</marc:subfield>
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    <marc:datafield tag="264" ind1=" " ind2="1">
      <marc:subfield code="a">[Ottawa] : </marc:subfield>
      <marc:subfield code="b">Geological Survey of Canada, </marc:subfield>
      <marc:subfield code="c">2023.</marc:subfield>
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      <marc:subfield code="c">©2023</marc:subfield>
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      <marc:subfield code="a">1 online resource (18 pages) : </marc:subfield>
      <marc:subfield code="b">colour illustrations, maps (some colour).</marc:subfield>
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      <marc:subfield code="a">online resource</marc:subfield>
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      <marc:subfield code="a">Open file, </marc:subfield>
      <marc:subfield code="x">2816-7155 ; </marc:subfield>
      <marc:subfield code="v">8985</marc:subfield>
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      <marc:subfield code="a">Includes bibliographical references (pages 14-18).</marc:subfield>
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      <marc:subfield code="a">"The inversion of new compilations of aeromagnetic data and gravity data are employed to investigate the 3-D physical property (magnetic susceptibility and density) distribution within the Great Bear magmatic zone. The application of two different software suites (Geosoft VOXI and UBC GIF MAG3D and GRAV3D) affords a comparison of approaches and results. The magnetic susceptibility results are broadly compatible, but Geosoft VOXI enabled more detailed definition of shallow sources, due to the lower upward continuation required for a resulting smooth model. The density results were markedly different in how the model responded to the low-resolution gravity data, in characterization of the near-surface. GRAV3D extrapolated shallow sources to surface, whereas Geosoft VOXI smoothed and closed the top of shallow sources below surface. The different magnetic susceptibility and density models can be used to assess the physical property distribution and relationships across the region. One approach, applied here, is to combine the near-surface magnetic susceptibility and density results to identify zones of coincidently high physical properties, a common physical property relationship associated with IOCG mineral deposits. These integrated models highlight many of the region's known mineral occurrences and reveal other zones for further analysis"--Abstract, page 1.</marc:subfield>
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      <marc:subfield code="a">Magnetic anomalies</marc:subfield>
      <marc:subfield code="z">Northwest Territories.</marc:subfield>
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      <marc:subfield code="a">Gravity anomalies</marc:subfield>
      <marc:subfield code="z">Northwest Territories.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="0">
      <marc:subfield code="a">Inversion (Geophysics)</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="6">
      <marc:subfield code="a">Anomalies magnétiques</marc:subfield>
      <marc:subfield code="z">Territoires du Nord-Ouest.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="6">
      <marc:subfield code="a">Anomalies de la pesanteur</marc:subfield>
      <marc:subfield code="z">Territoires du Nord-Ouest.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="6">
      <marc:subfield code="a">Inversion (Géophysique)</marc:subfield>
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      <marc:subfield code="a">Geological Survey of Canada, </marc:subfield>
      <marc:subfield code="e">issuing body.</marc:subfield>
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      <marc:subfield code="a">Open file (Geological Survey of Canada)</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
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      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-2/M183-2-8985-eng.pdf</marc:subfield>
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      <marc:subfield code="u">https://doi.org/10.4095/331954</marc:subfield>
      <marc:subfield code="z">(complete dataset)</marc:subfield>
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