CRC LEME  
              Open File Report 157: 
              ABSTRACT
             
            Teilta regolith project: Basement modelling
            L. Ruperto
            
              The basement modelling research initiative, which is part of 
                the Teilta regolith project of CRC LEME Project 2.1, involved 
                the development and construction of a 3D depth to basement model 
                over the area covered by the Teilta 1:100,000 topographic map 
                sheet. This arid landscape, located just to the north of the Broken 
                Hill Domain, is dominated by Proterozoic bedrock overlain by various 
                regolith units. The 3D model is able to provide a visual insight 
                into the form and nature of the subsurface environment, in particular 
                visualising the subsurface configuration of the Palaeoproterozoic 
                Willyama basement under cover. The data used for this project, 
                although forming a relatively small dataset, was collected from 
                two major sources: (1) drillhole intersections as collated by 
                New South Wales Department of Mineral Resources, and (2) ground 
                observations of bedrock outcrops collated by Steve Hill from Adelaide 
                University. Following a number of spatial adjustments required 
                to fit the data to the topography, a variety of GIS products (such 
                as contours maps, interpolated grids, point datasets) were generated 
                and form the foundations of the 3D depth to basement model. The 
                model allows for visualisation of the topographic surface combined 
                with the interpreted location of the basement as it would appear 
                in the actual environment in three dimensions. This allows the 
                viewer to examine the model in a full 360° range of motion, 
                including enabled zoom in/out features. The 3D model is able to 
                identify areas where bedrock crops out at the topographic surface 
                or where it is only very shallow below that surface, while also 
                displaying significantly deeper bedrock distribution within the 
                map sheet area.  
                
            
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