<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Weyer, K.U.</style></author><author><style face="normal" font="default" size="100%">Ellis, J.C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact of groundwater dynamics on the genesis of the Athabasca Oil sands-A novel approach</style></title><secondary-title><style face="normal" font="default" size="100%">First EAGE/TNO Workshop</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">groundwater dynamics</style></keyword><keyword><style  face="normal" font="default" size="100%">low fluid dynamic drain</style></keyword><keyword><style  face="normal" font="default" size="100%">Palaeozoic karst</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">05/2015</style></date></pub-dates></dates><abstract><style face="normal" font="default" size="100%">The regional groundwater dynamics caused by the “low fluid dynamic drain” (Hitchon, 1969) is associated with flow through highly permeable karst. The amounts of winter discharge from the Paleozoic karst into the Athabasca River allows the estimation of the rate of groundwater with oxygen annually penetrating the oil sands layer. The associated oxygen and biodegradation are assumed to be important agents for the transformation of oil into heavy oil and tar. The paper puts emphasis on the often-neglected impact of groundwater dynamics on geochemical processes. </style></abstract><custom2><style face="normal" font="default" size="100%">Athabasca River</style></custom2></record></records></xml>