\(t=exp[-E(m*)/T)]/exp[-E(m(p)/T)]=exp[-[E(m*)-Em(p)]/T]\)

5 Results

    After giving 2000 iterations to the Monte Carlo inversion approach we got estimates for the model parameters for the density contrast as 6567 kgm-3 and 26.5 km as the source depth of the Covington pluton (fig.4a, 4b). The estimates had a minimum error of 0.2 X 10-4 with a similar distribution for the predicted and observed gravity anomaly (fig.4c).