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    <marc:controlfield tag="001">9.956505</marc:controlfield>
    <marc:controlfield tag="003">CaOODSP</marc:controlfield>
    <marc:controlfield tag="005">20251113071927</marc:controlfield>
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      <marc:subfield code="a">Pe-Piper, G., </marc:subfield>
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    <marc:datafield tag="245" ind1="1" ind2="0">
      <marc:subfield code="a">Detrital mineral provenance analyses from the Cretaceous McMurray Formation, Alberta and the Holocene Portneuf river delta, North Shore of Quebec / </marc:subfield>
      <marc:subfield code="c">G. Pe-Piper, D.J.W. Piper, A. Blowick, G. Gomez Garcia, K. Wallace, and C. Sangster.</marc:subfield>
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      <marc:subfield code="a">[Ottawa] : </marc:subfield>
      <marc:subfield code="b">Natural Resources Canada = Ressources naturelles Canada, </marc:subfield>
      <marc:subfield code="c">2021.</marc:subfield>
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      <marc:subfield code="c">©2021</marc:subfield>
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      <marc:subfield code="a">1 online resource (391 pages) : </marc:subfield>
      <marc:subfield code="b">illustrations (some colour), colour maps.</marc:subfield>
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      <marc:subfield code="a">computer</marc:subfield>
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      <marc:subfield code="2">rdamedia</marc:subfield>
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      <marc:subfield code="a">online resource</marc:subfield>
      <marc:subfield code="b">cr</marc:subfield>
      <marc:subfield code="2">rdacarrier</marc:subfield>
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      <marc:subfield code="a">Geological Survey of Canada open file, </marc:subfield>
      <marc:subfield code="x">2816-7155 ; </marc:subfield>
      <marc:subfield code="v">8761</marc:subfield>
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      <marc:subfield code="a">ISSN of series supplied from ISSN Portal.</marc:subfield>
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    <marc:datafield tag="504" ind1=" " ind2=" ">
      <marc:subfield code="a">Includes bibliographical references (pages 26-30).</marc:subfield>
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      <marc:subfield code="a">"The dispersion of sandy sediment by the early Cretaceous Sable River has been further investigated by detailed mineralogical study of (a) two samples from the Aptian McMurray Formation of Alberta and (b) a Holocene deltaic deposit on the North Shore of the St Lawrence Estuary. Samples from Alberta were to test the hypothesis that Aptian diversion of the Sable River led to it flowing to the Western Interior Seaway, contributing sand to the McMurray Formation. Pb-isotopes in K-feldspar show that most of the first cycle feldspars in the McMurray Formation were derived from the local Trans-Hudson Orogen. The heavy mineral assemblage, particularly the abundance of staurolite and paucity of chromite, is different from that of the Sable River. The Holocene deltaic sand was analysed to identify distinctive heavy minerals from that part of the Grenville terrane. Garnets are similar to enigmatic garnets from the Jurassic of the Mohawk B-93 well, where Pb-isotopes on K-feldspar also suggest a Grenville source. Titania minerals with abundant quartz inclusions, known from both the Scotian Basin and the McMurray Formation, were not present in the Holocene sample and their provenance significance remains enigmatic"--Abstract, page 5.</marc:subfield>
    </marc:datafield>
    <marc:datafield tag="650" ind1=" " ind2="0">
      <marc:subfield code="a">Sediments (Geology)</marc:subfield>
      <marc:subfield code="z">Alberta</marc:subfield>
      <marc:subfield code="z">McMurray Formation</marc:subfield>
      <marc:subfield code="x">Analysis.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="0">
      <marc:subfield code="a">Sediments (Geology)</marc:subfield>
      <marc:subfield code="z">Québec (Province)</marc:subfield>
      <marc:subfield code="z">Côte-Nord</marc:subfield>
      <marc:subfield code="x">Analysis.</marc:subfield>
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      <marc:subfield code="a">Mineralogy, Determinative</marc:subfield>
      <marc:subfield code="z">Alberta</marc:subfield>
      <marc:subfield code="z">McMurray Formation.</marc:subfield>
    </marc:datafield>
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      <marc:subfield code="a">Mineralogy, Determinative</marc:subfield>
      <marc:subfield code="z">Québec (Province)</marc:subfield>
      <marc:subfield code="z">Côte-Nord.</marc:subfield>
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    <marc:datafield tag="650" ind1=" " ind2="6">
      <marc:subfield code="a">Sédiments (Géologie)</marc:subfield>
      <marc:subfield code="z">Alberta</marc:subfield>
      <marc:subfield code="z">McMurray, Formation de</marc:subfield>
      <marc:subfield code="x">Analyse.</marc:subfield>
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      <marc:subfield code="a">Sédiments (Géologie)</marc:subfield>
      <marc:subfield code="z">Québec (Province)</marc:subfield>
      <marc:subfield code="z">Côte-Nord</marc:subfield>
      <marc:subfield code="x">Analyse.</marc:subfield>
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      <marc:subfield code="a">Minéralogie déterminative</marc:subfield>
      <marc:subfield code="z">Alberta</marc:subfield>
      <marc:subfield code="z">McMurray, Formation de.</marc:subfield>
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      <marc:subfield code="a">Minéralogie déterminative</marc:subfield>
      <marc:subfield code="z">Québec (Province)</marc:subfield>
      <marc:subfield code="z">Côte-Nord.</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>
      <marc:subfield code="v">8761.</marc:subfield>
      <marc:subfield code="w">(CaOODSP)9.506878</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">286.00 MB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-8761-eng.pdf</marc:subfield>
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      <marc:subfield code="q">HTML</marc:subfield>
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      <marc:subfield code="u">https://doi.org/10.4095/327838</marc:subfield>
      <marc:subfield code="z">Complete dataset</marc:subfield>
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