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| 001 | 9.842179 |
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| 003 | CaOODSP |
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| 005 | 20230131161138 |
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| 007 | cr ||||||||||| |
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| 008 | 170822s2017 oncabd ob f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 043 | |an-cn-nu |
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| 086 | 1 |aM183-2/7895E-PDF |
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| 100 | 1 |aAnand, Arvind. |
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| 245 | 10|aReactivated fault systems and their effects on outcrop patterns of thin-skinned early thrust imbrications in the Kiggavik uranium camp, Nunavut |h[electronic resource] / |cA. Anand and C.W. Jefferson. |
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| 260 | |a[Ottawa] : |bNatural Resources Canada, Geological Survey of Canada, |c2017. |
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| 300 | |a1 p. : |bcol. charts, col. ill., col. maps + |ebibliographical references (9 p.), 7 maps (figures 1-3, 5-7) |
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| 490 | 1 |aGeological Survey of Canada, open file ; |v7895 |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"Intersecting faults in the northeast Thelon Basin region were investigated under the Geomapping for Energy and Minerals Program in order to understand their effects on outcrop patterns, and their potential spatial relationships to uranium (U) deposits. Existing and new data were compiled and interpreted to produce maps that respect all observations. An important structural complex that existed long before the reactivated faults and filling of the Thelon Basin is a stack of repeated a) greywacke, b) rhyolite and c) quartzite that overlies a number of uranium deposits and prospects. This near-horizontal stack was broken into small segments by intersecting near-vertical reactivated faults, resulting in discontinuous outcrops that line up poorly. The stack formed an impermeable layer but the cross cutting faults, especially their intersections, created zones down which hot water could have easily flowed to produce the deep accumulations of U oxide minerals"--Summary provided by publisher. |
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| 692 | 07|2gccst|aStructural geology |
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| 692 | 07|2gccst|aGeophysics |
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| 692 | 07|2gccst|aMinerals |
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| 692 | 07|2gccst|aGeological maps |
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| 700 | 1 |aJefferson, Charles Wilson,|d1949- |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aOpen file (Geological Survey of Canada)|v7895|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s161.36 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-eng.pdf|zOpen File 7895 |
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| 856 | 40|qPDF|s90 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-1-eng.pdf|zOpen File 7895 references |
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| 856 | 40|qPDF|s849 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-2-eng.pdf|zFigure 1 |
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| 856 | 40|qPDF|s4.62 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-3-eng.pdf|zFigure 2A |
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| 856 | 40|qPDF|s17.17 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-4-eng.pdf|zFigure 2B |
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| 856 | 40|qPDF|s10.59 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-5-eng.pdf|zFigure 3 |
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| 856 | 40|qPDF|s34.18 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-6-eng.pdf|zFigure 5 |
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| 856 | 40|qPDF|s37.30 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-7-eng.pdf|zFigure 6 |
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| 856 | 40|qPDF|s18.91 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-7895-8-eng.pdf|zFigure 7 |
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