The Inversion Of The Data In The Modeling (South West Of Kuhpayeh)

Geometry and topography of the bedrock of the area can be recognized by the difference between optimal density and the density of the bedrock, in which all of the calculation for determining the topography of the bedrock are performed in the Fourier area. In fact, all of the obtained results are approximately good in geology and the drilled exploratory in determining topography of the area’s bedrock.