MAPPING SURFACE GEOCHEMICAL DATA WITH GIS IN LOWER LISBON VALLEY, UTAH
The LVMC lies on the eastern portion of the Colorado Plateau region within the section overlying the Paradox Basin. Structurally, the mine sits in the collapsed flank of a salt anticline with ore trends following normal faults in the section above salt. Deeper faults likely provided conduits for copper-rich fluids derived from Pennsylvanian sediments. Current mining operations exploit hypogene chalcocite with lesser amounts of bornite and chalcopyrite in sandstones and conglomerates of the Cretaceous Burro Canyon and Dakota formations. In Lower Lisbon Valley (LLV) economic mineralization thus shows both stratigraphic and structural control.
Exploration has started further southeast from the mine along the faulted margins of the valley. Soil and anthill samples in the exploration areas were analyzed by ICP-MS, and concentrations were plotted using heat maps in GIS. Similarities between the anthill and soil samples were identified. All sampling techniques revealed higher concentrations of copper near the major normal faults associated with salt-anticline collapse, and the extension of structural control. Optimized heat maps based off conversion of bulk composition to point data illustrates prospects in LLV as viable options for economic extraction of copper.