Structures and Faults in the Peace River Arch Region, Alberta, 2006 (GIS Data, line features)

Structures and Faults in the Peace River Arch Region, Alberta, 2006 (GIS Data, line features) This GIS data set depicts the faults in the Peace River Arch Region, based on petroleum well log data including formation picks. Well data were sourced from Accumap and EUB data sets. These faults are interpreted from structure top residual surfaces generated by the removal of geological trend. The geological trend was modelled using geostatistical analysis to highlight local offset in multiple, easily recognizable formation tops.The stratigraphic interval considered was from the Cretaceous down to the top of the PreCambrian. 2022-04-13 Government of Alberta AGS-Info@aer.ca Form DescriptorsNature and EnvironmentScience and Technology83m83n84c84d84e84f84lalbertacanadafaultgeologygeoscientificinformationgis datapeace river archpeace river areastratigraphicstructureswestern canada sedimentary basinGovernment information Structures and Faults in the Peace River Arch Region, Alberta, 2006 (GIS Data, line features) - (HTML)HTML https://geodiscover.alberta.ca/geoportal/rest/metadata/item/0054436b9913471ab61e32ab910be7eb/html Structures and Faults in the Peace River Arch Region, Alberta, 2006 (GIS Data, line features) - (SHP)SHP https://static.ags.aer.ca/files/document/DIG/DIG_2007_0011.zip Structures and Faults in the Peace River Arch Region, Alberta, 2006 (GIS Data, line features) - (XML)XML https://geodiscover.alberta.ca/geoportal/rest/metadata/item/0054436b9913471ab61e32ab910be7eb/xml Alberta GeoportalHTML https://open.alberta.ca/opendata/d21e6b54-4dfb-4285-b658-7c6612a83c48

This GIS data set depicts the faults in the Peace River Arch Region, based on petroleum well log data including formation picks. Well data were sourced from Accumap and EUB data sets. These faults are interpreted from structure top residual surfaces generated by the removal of geological trend. The geological trend was modelled using geostatistical analysis to highlight local offset in multiple, easily recognizable formation tops.The stratigraphic interval considered was from the Cretaceous down to the top of the PreCambrian.

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