Transfer Function Identification using CLM Techniques

Using a mathematical model that was developed to predict microseismic signals in various terrains and the closed loop methodology (CLM), geological transfer functions were determined using data obtained from seismic tests. The earth transfer function was assumed to be comprised of two components. These components consisted of the source coupling and R-wave transmission coefficients. Using data obtained from test information and model predicts of these coefficients, this paper shows how the actual coefficients for a site can be obtained.