By Stephen P. Klein
In may well 1998, Rudolph W. Giuliani, the mayor of recent York urban, convened The Mayor's Advisory activity strength at the urban college of recent York (CUNY). the duty strength requested the Council for reduction to schooling, a subsidiary of RAND, to behavior an autonomous research of a number of features of CUNY's rules and methods. This document is the second one in a sequence of news in this paintings.
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Additional resources for CUNY's Testing Program: Characteristics, Results and Implications for Policy and Research
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.