Mapping the geothermal anomaly on the island of Milos/Greece by magneto-tellurics
Audiomagnetotelluric and magnetotelluric measurements have been performed on the island of Milos. Importance is attached to robust processing techniques and to the distortion problem at longer periods. The geothermal anomaly displays extremely low resistivities (0.2 ohm.m) at 10 Hz, which corresponds to the upper 200m. The central anomaly is still seen at periods around 1000s. The joint mapping of apparent resistivity by all groups participating in the experiment indicates the detailed outlines of the anomaly.
Bibliographic Reference: EUR 12247 EN (1990) 305 pp., MF, ECU 16
Record Number: 199010159 / Last updated on: 1994-12-01
Original language: en
Available languages: en