@article {schneiderstructural,
	title = {Structural deformation and karst in the Devonian waterways formation: examples from outcrops along the Athabasca River},
	year = {2014},
	pages = {4 pages },
	abstract = {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.
},
	keywords = {breccia, green clay, karst, paleokarst, sandstone fill},
	url = {http://cseg.ca/assets/files/resources/abstracts/2014/215_GC2014_Structural_Deformation_and_Karst_in_the_Devonian_Waterways_Fm.pdf},
	author = {Schneider, Chris L and Grobe, Matthias}
}
