Search
Now showing items 1-1 of 1
Geochemical and isotopic tracing of Paleozoic groundwater flow in breached anticlines : a case study at Lower Kane Cave, Bighorn Basin, Wyoming
(2004-08-16)
Lower Kane Cave is forming in the upper Mississippian Madison Limestone by sulfuric acid speleogenesis. The cave is located along the axialtrace of the Little Sheep Mountain anticline where the Paleozoic units have been ...