Magnetotellurics (MT) Services

At a basic level of interpretation, resistivity is correlated with different rock types. High-velocity layers are typically highly resistive, whereas sediments - porous and permeable - are typically much less resistive. While high-velocity layers are an acoustic barrier and make seismic ineffective, their electrical resistivity means the magnetic signal passes through almost unimpeded. This allows MT to see deep beneath these acoustic barrier layers, complimenting the seismic data and assisting interpretation.

A highly reflective layer of dense Cenozoic rocks forms an acoustic barrier at a depth of about 1km. Seismic methods produce almost no information below this layer, as shown on the cross-section at left. MT exploration, however, clearlyshowed the presence of the oil-prospective layers in the Upper Paleozoic rocks.