Interpretation of magnetic anomalies due to dikes; the complex gradient methodD. Atchuta Rao, P. Narayan, H. V. Ram Babu|Geophysics|1981Cited by 107
Relationship of magnetic anomalies due to subsurface features and the interpretation of sloping contactsD. Atchuta Rao, P. Narayan, H. V. Ram Babu|Geophysics|1980Cited by 22
Interpretation of the total magnetic intensity anomaly due to a two-dimensional asymmetrical triangular prism using Fourier transformsH. V. Ram Babu, P. Narayan, D. Atchuta Rao|Geoexploration|1980Cited by 2