As a part of the ''Deep-Seated Geothermal Resources Survey (DSGR)'' pr
oject being undertaken by the New Energy and Industrial Technology Dev
elopment Organization (NEDO), the ''Vertical Electro Magnetic Profilin
g (VEMP)'' method is being developed to accurately obtain deep resisti
vity structures. The VEMP method takes multi-frequency three-component
magnetic field data in an open hole well using controlled source tran
smitters emitted at the surface (either loop or grounded-wire sources)
, Numerical simulations using EM3D have demonstrated that phase data o
f the VEMP method is not only very sensitive to the general resistivit
y structure, but will also indicate the presence of deeper anomalies.
Forward modelling was used to determine the required transmitter momen
ts for various grounded-wire and loop sources for a field test using t
he WD-1 well in the Kakkonda geothermal area. VEMP logging of the WD-1
well was carried out in May 1994 and the processed field data matches
the computer simulations quite well.