<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Schneider, Chris L</style></author><author><style face="normal" font="default" size="100%">Grobe, Matthias</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Structural deformation and karst in the Devonian waterways formation: examples from outcrops along the Athabasca River</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">breccia</style></keyword><keyword><style  face="normal" font="default" size="100%">green clay</style></keyword><keyword><style  face="normal" font="default" size="100%">karst</style></keyword><keyword><style  face="normal" font="default" size="100%">paleokarst</style></keyword><keyword><style  face="normal" font="default" size="100%">sandstone fill</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://cseg.ca/assets/files/resources/abstracts/2014/215_GC2014_Structural_Deformation_and_Karst_in_the_Devonian_Waterways_Fm.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">4 pages </style></pages><abstract><style face="normal" font="default" size="100%">Structural deformation and karst are frequent phenomena of Devonian outcrops along the Athabasca River in northeastern Alberta. Folds, joints, and, less so, evidence of movement along fractures are ubiquitous; karst features are less common and often subtle. Evidence of paleokarst includes green clay, breccia, and sandstone fill, often in fractures, and less commonly, caves and solution-enlarged joints.
</style></abstract><custom2><style face="normal" font="default" size="100%">Athabasca River</style></custom2></record></records></xml>