Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XL-8, 469-476, 2014
http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-8/469/2014/
doi:10.5194/isprsarchives-XL-8-469-2014
© Author(s) 2014. This work is distributed
under the Creative Commons Attribution 3.0 License.
 
28 Nov 2014
GIS based 3D visualization of subsurface and surface lineaments / faults and their geological significance, northern tamil nadu, India
J. Saravanavel and S. M. Ramasamy Centre for Remote Sensing, Bharathidasan University, Tiruchirappalli, Tamil Nadu, India
Keywords: GIS based 3D visualization, Subsurface lineaments, Surface lineaments, Northern Tamil Nadu, India Abstract. The study area falls in the southern part of the Indian Peninsular comprising hard crystalline rocks of Archaeozoic and Proterozoic Era. In the present study, the GIS based 3D visualizations of gravity, magnetic, resistivity and topographic datasets were made and therefrom the basement lineaments, shallow subsurface lineaments and surface lineaments/faults were interpreted. These lineaments were classified as category-1 i.e. exclusively surface lineaments, category-2 i.e. surface lineaments having connectivity with shallow subsurface lineaments and category-3 i.e. surface lineaments having connectivity with shallow subsurface lineaments and basement lineaments. These three classified lineaments were analyzed in conjunction with known mineral occurrences and historical seismicity of the study area in GIS environment. The study revealed that the category-3 NNE-SSW to NE-SW lineaments have greater control over the mineral occurrences and the N-S, NNE-SSW and NE-SW, faults/lineaments control the seismicities in the study area.
Conference paper (PDF, 2604 KB)


Citation: Saravanavel, J. and Ramasamy, S. M.: GIS based 3D visualization of subsurface and surface lineaments / faults and their geological significance, northern tamil nadu, India, Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XL-8, 469-476, doi:10.5194/isprsarchives-XL-8-469-2014, 2014.

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