of the traditional smooth inversion this information is provided as [2J The two-dimensional (2-D) magnetotelluric inverse problem an assumption that the solution, the geoelectrical model in the MT has been addressed by several authors. The most well-known case, should be represented by smooth functions. At the same time, approaches are the search for a smooth model [de Groot-Hedlin in some geol...

Pertamina has conducted geothermal exploration in Sumatra showing that the depths to the top of most of the geothermal reservoirs are about 1000-2000 meters. Previous geophysical exploration work by Pertamina emphasized the use of DC-resistivity methods such as the Schlumberger method. However, these techmques can typically only penetrate to a depth of less than 1000 meters and are too shallow ...

J. Alvarez-Aramberri∗, D. Pardo and H. Barucq ∗ University of the Basque Country (UPV/EHU), Bilbao, Spain, Inria team-project Magique-3D, and LMA UMR 5142 UPPA, Pau, France, [email protected], https://sites.google.com/site/m2sigroup/. 2 Department of Applied Mathematics, Statistics, and Operational Research at the University of the Basque Country (UPV/EHU), and IKERBASQUE, Basqu...

Abstract This paper presents a Multidisciplinary geophysical study of the geothermal areas in Uzbekistan. Based on developed new map, data anomalous were analyzed. Muruntau area, comprehensive methodology has been for detailing anomalies. New integrated surveys (gravity survey, seismic magnetotelluric survey) and their interpretation at stage exploration are presented.