{ "culture": "en-US", "name": "", "guid": "", "catalogPath": "", "snippet": "The feature class was created to illustrate the thickness of Quaternary sediment, north of latitude 56. These contours are generated from calculated values between surface objects (Top of Quaternary and Base of Quaternary) produced in Paradigm\u2019s SKUA-GocadTM software. Contours are set to 20 m increments. They are exported as a DXF file and then imported into ESRI software where the feature class is created.", "description": "

The surface objects, \u2018Top of Quaternary\u2019 and \u2018Base of Quaternary\u2019, used to calculate the isopach thickness of the Quaternary, were modelled using the following data. <\/SPAN><\/SPAN><\/P>

  1. Drillhole information (>11 500 drillholes)<\/SPAN><\/SPAN><\/P><\/LI>

  2. Depth information from provincial lake sediment data (>14 000 lake depths)<\/SPAN><\/SPAN><\/P><\/LI>

  3. Outcrop data (>4600 outcrops) \u2013 zero edges for Quaternary material<\/SPAN><\/SPAN><\/P><\/LI>

  4. Depth information from scanned bathymetric maps (40 lakes)<\/SPAN><\/SPAN><\/P><\/LI>

  5. Lake sediment, bathymetric and seismic data points (~130 000) from industry assessment files (SMAD database)<\/SPAN><\/SPAN><\/P><\/LI><\/OL>

    Outcrop data inside the Athabasca basin boundary comes from a compilation of outcrop polygons from various mapping projects and industry reports; the compilation of outcrop polygons is available on GeoAtlas. Outcrop data from outside the Athabasca basin boundary, includes bedrock polygons from 1 million-scale compilation maps from Alberta (Fenton et al., 2013) and Saskatchewan (Simpson, 1997) were used. These bedrock regions, outside the basin, may have sporadic or thin (generally <2 m) Quaternary cover; however, the modelling of this surface assumed there was none.<\/SPAN><\/SPAN><\/P>

    <\/P><\/DIV><\/DIV><\/DIV>", "summary": "The feature class was created to illustrate the thickness of Quaternary sediment, north of latitude 56. These contours are generated from calculated values between surface objects (Top of Quaternary and Base of Quaternary) produced in Paradigm\u2019s SKUA-GocadTM software. Contours are set to 20 m increments. They are exported as a DXF file and then imported into ESRI software where the feature class is created.", "title": "Quaternary Isopach Contours (North of latitude 56*N) of Saskatchewan, Canada, Saskatchewan Geological Survey, UTM NAD83 Zone 13", "tags": [ "quaternary", "icopach", "thickness", "drift" ], "type": "", "typeKeywords": [], "thumbnail": "", "url": "", "minScale": 150000000, "maxScale": 5000, "spatialReference": "", "accessInformation": "Bosman, S.A., Paiement, J.-P., Williston, C. and Card, C.D. (2020): Development of Athabasca 3-D model 2.0; in Summary of Investigations 2020, Volume 2, Saskatchewan Geological Survey, Saskatchewan Ministry of Energy and Resources, Miscellaneous Report 2020-4.2, Paper A-3, 14p.\n\nBosman, S.A., Paiement, J.-P., Williston, C. and Mahmoodi, O. (2020): Athabasca 3-D model 2.0; Saskatchewan Ministry of Energy and Resources, Saskatchewan Geological Survey, 3-D File.", "licenseInfo": "

    Although the Ministry has exercised all reasonable care in the compilation, interpretation, and production of this item, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Ministry and the Government of Saskatchewan do not accept liability for any errors, omissions, or inaccuracies that may be included in or derived from, this item.<\/SPAN><\/SPAN><\/P>

    <\/P><\/DIV><\/DIV><\/DIV>" }