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• W1552023365 abstract "Abstract The visualization of three dimensional structure from two dimensional maps is greatly complicated by topographic relief. Digital Terrain Models (DTM), within a Geographic Information System (GIS) can significantly enhance the visual impact of a complexly deformed terrain. A DTM allows the viewing of landscape surfaces, from any vantage point, with geology, satellite imagery, or any two-dimensional map image draped over the surface. Data point representation as a Triangulated Irregular Network (TIN), involves the modelling of a surface as a sheet of triangular facets having data points as their vertices; thereby, honouring variable topography without data redundancy since the triangular mesh adapts to varying densities of data. All critical topographic features are thereby retained. The demonstrated data set is that of the Pingston Fold within the Monashee Mountains of southeastern British Columbia, Canada. The Pingston Fold is situated in the Thor-Odin structural culmination of the Monashee Complex, within the Omineca Belt of the Canadian Cordillera. The Pingston Fold is a major complex structural feature outcropping in the southern half of the Thor-Odin culmination. The structural interpretation is based on an orthographic projection of the Digital Terrain Model. It was produced by first dividing the map into fold domains defined on the basis of homogeneity of the orientations of fold axes where reasonably cylindrical ( i.e., where poles to the folded gneissosity plot as a great circle girdle). Once structural domains have been outlined on a map, all data can be projected down plunge and the structure joined at domain boundaries. This differs from conventional manual plotting in that all data points are projected from their position on the modelled topographic surface, rather than from a planar surface of a block. This makes a significant difference in such mountainous terrains. The present surface expression and the three-dimensional geometry of the Pingston Fold can be explained by fold interference and the structure is illustrated using a Digital Terrain Model." @default.
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• W1552023365 date "1996-01-01" @default.
• W1552023365 modified "2023-09-26" @default.
• W1552023365 title "Digital Terrain Models and the Visualization of Structural Geology" @default.
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• W1552023365 doi "https://doi.org/10.1016/s1874-561x(96)80032-0" @default.
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