B. Tournerie et al., INVERSION OF THE COPROD2 MAGNETOTELLURIC DATA USING A DIFFUSIVE-TO-PROPAGATIVE MAPPING (DPM), Geophysical research letters, 22(16), 1995, pp. 2187-2190
Diffusive-to-Propagative Mapping (DPM) transforms a diffusive electrom
agnetic field into a dual wave field to produce electromagnetic reflec
tivity images similar to non-migrated seismic sections. An application
of DPM to the COPROD2 data set gives reflectivity images showing thre
e distinct reflectors attributed to resistivity jumps located at depth
s ranging from 2 to 50 km. The deeper reflector may be related to a ma
jor west-dipping seismic reflector detected with the COCORP seismic da
ta.