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Pakistan and its neighboring counties comprise all famous forms of most crucial plate limitations in addition to very important dynamic intra-plate twists. realizing the tectonics during this multifaceted zone has been behind schedule by way of a relative loss of info and the trouble of geologic and tectonic problems. inspite of the increase within the volume of knowledge some time past few years, the issues of the world want a multidirectional method of do something about the geology and tectonics. therefore, as a way to gather large, multidirectional information units with various superiority and backbone, this research takes on a Geographic details method (GIS) method of see at those issues in a accomplished and unparalleled manner. during this examine, the authors assemble maps of surficial tectonic positive factors and deepness of the Moho, Pn velocities and Pg velocities for Pakistan and clarify a cross-section capacity to paintings with information in a GIS layout.

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Upwelling asthenosphere beneath western Arabia and its regional implications, J. Geophy. 15255-15271. Chaimov, T. , 1990. 1369-1386. , 1994. Spatial analysis of lineaments. 1237-1258. , 1984. Structural Geology of rocks and regions. 475. , 1930. Geological work of the Italian expedition to the Karakoram. Geographical Journal, 75,pp. 402-411. Dewey, J. , 1979. Aegean and surrounding regions: complex multiple and continuum tectonics in a convergent zone. Geol. Soc. Am. Bull. 84-92. , Amada, T. & Aniya, M.

Geophy. 15255-15271. Chaimov, T. , 1990. 1369-1386. , 1994. Spatial analysis of lineaments. 1237-1258. , 1984. Structural Geology of rocks and regions. 475. , 1930. Geological work of the Italian expedition to the Karakoram. Geographical Journal, 75,pp. 402-411. Dewey, J. , 1979. Aegean and surrounding regions: complex multiple and continuum tectonics in a convergent zone. Geol. Soc. Am. Bull. 84-92. , Amada, T. & Aniya, M. 2000. Landslide hazard mapping and its evaluation using GIS: an investigation of sampling schemes for a gridcell based quantitative method.

Conversely Kashmir and northern Punjab contains relatively less values than the northern part of study area. Southern Punjab and central Balochistan have moderate value of moho depth. The lower most part of study area is costal zone having lowest values of moho depth. Due to non-availability of moho depth data in the Badin district the area is left blank 44 45 Figure 6. 8 are seismotectonic GIS of Pakistan. 6, is geographical, geological and Pn velocity. In the other two maps Pg velocity and moho depth data have been used with geographical and geological data sets of study area.

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