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• W3144440929 abstract "Received 1984 May 8; in original form 1983 July 1 I Summary. The methods of magnetotelluric (MT) and differential geomagnetic soundings (DGS) have been applied to study the electromagnetic response of the structure of the Senegal sedimentary basin. The measurements at 10 sites were carried out along a profile running perpendicularly across a zone of north-south flexures and faults over the period range 10-1000 s. Variation of periods up to 10000 s were obtained at two sites. The anomalous geomagnetic variation field across the major fault zone is characterized by an increase in the magnetic eastward component. Two-dimensional modelling of the apparent resistivities and phases reveals a highly anomalous upper crustal structure involving a low-resistivity zone in the central part of the basin (less than 30 am). To satisfy the additional long-period data at two sites, a deep conductor is also required at a depth below 300 km with a resistivity less than 10 am. The crustal discontinuity located - 200 km off the coast is possibly related to the opening of the Atlantic Ocean. The difficulty in resolving the question of the nature of the crust in this region" @default.
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• W3144440929 date "1984-01-01" @default.
• W3144440929 modified "2023-09-23" @default.
• W3144440929 title "Electrical resistivity structure of the Senegal basin as determined from magnetotelluric and differential geomagnetic soundings" @default.
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