Regional 3-D imaging of resistivity structure using GEMIT inversion

Mathematics – Logic

Scientific paper

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Scientific paper

The analysis of LANDSAT imageries has been studied in association of geodetic, gravitational, geomagnetic and electromagnetic structures. Those physical parameters however differ from each other in observational range and resolution. GEMIT (Geo-electromagnetic Induction Tomography) is one of the methods to visualize a conductivity structure by inversion of electromagnetic induced signals to a prefered conductor as an imagery pattern under the ground. Several features of volcanoes, geological faults, or seismic zones detected by satellite imagery analysis were examined from geophysical prospecting data. This report concerns to a practical case analyzed in the northern part of Japan, where the above mentioned topographic features were seen as extended to the conductivity structures at the deeper levels in the crust.

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