Pedersen, Per KentLeier, AndrewTullius, Dylan Neill2014-08-212014-11-172014-08-212014http://hdl.handle.net/11023/1690The Isachsen Formation is a Barremian to Aptian-aged fluvio-deltaic succession ranging in thickness from tens of meters to over 1400 m within the Sverdrup Basin of the Canadian Arctic Archipelago. The formation exhibits a variety of lithologies including coarse-grained quartz-arenite sandstones, fine-grained ripple laminated sandstones and siltstones, marine mudstones and coal deposits that were deposited in meandering, braided stream, coastal plain and shallow marine shelf depositional environments. This study classifies the Isachsen Formation as a mixture of recycled and craton derived sediments prograding northwest through the Sverdrup Basin with both source and reservoir potential in previously overlooked areas. Sedimentation during this time period was affected by active diapirism in some locations on Ellef Ringnes Island. Interpretations are based on observations from over 6,000 m of measured stratigraphic sections, local mapping of facies contacts, palynology, sandstone petrography and field sample studies trough geochemical and rock pyrolysis evaluation.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.GeologyMineralogyPalynologyIsachsenSverdrupCretaceousmaster thesis10.11575/PRISM/27890