Abstract
The paper presents the results of geophysical investigations carried out in the northernmost part of the Khetri Copper Belt, Rajasthan. The area investigated is a part of a Precambrian terrain consisting of a group of parametamorphites belonging to the Delhi System. The ore localisation is primarily controlled by fractures and shear zones consequent to faults located mostly along the contact of different lithologie units. The mineralisation is restricted essentially in the basal Ajabgarh or at the contact between the Ajabgarhs and the Alwars. The significance of the geophysical anomalies having distinct bearing with the various aspects of mineralisation has been discussed. A buried extension of the mineralised zone was established from the results of geophysical surveys (SP, magnetic and resistivity).
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