Abstract

Summary Audio magnetotelluric (AMT) and magnetotelluric (MT) studies were carried out in the western part of Bakreswar geothermal region covering an area of 330 square km. Apparent resistivity maps obtained from the AMT results delineated a well defined conducting zone at lower frequencies. AMT survey in the vicinity of Bakreswar hot spring (BHS) shows that there is no deep geoelectrical structure near the hot spring which can act as the source of Bakreswar hydrothermal system. Both AMT and MT results confirm the location of a major electrically conducting zone of considerable importance.

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