Bentley, LaurenceZhi, Lei2013-09-242013-11-122013-09-242013http://hdl.handle.net/11023/1014The petrophysical statistics of Paskapoo Formation lithologies were established from five Alberta Geological Survey boreholes after the lithologies were reclassified into a smaller set of groups. The study focused on gamma, density, resistivity, and sonic logs. Results show that 92 API and 19 ohm.m is the gamma and resistivity cutoff between sandstone and mudrock, and indicate that electrical resistivity method can be used to distinguish lithology of the Paskapoo Fm., while seismic refraction method has limited usage. Electrical resistivity and seismic refraction data were collected in a field site, Priddis, Alberta and processed to test the feasibility of the two methods to constrain the subsurface architecture. With the assistance from Priddis borehole and the combined interpretation of the two tomograms, results show the depth to the bedrock ranges from 5 to 10 m and heterogeneous upper part of the bedrock is dominated by sandstone and mudrock.engUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.GeophysicsPaskapoo FormationERTSeismic Refractionmaster thesis10.11575/PRISM/26293