Tutorial : 2-D and 3-D electrical imaging surveys

Beneath the old continental nuclei are thick root zones which translate coherently during plate motions. These zones are apparently stabilised against convective disruption by the depletion of the continental upper mantle in a basalt-like component. Construction of this delicately balanced tectosphere is accomplished by the dynamic and magmatic processes of the Wilson cycle.

Composition and development of the continental tectosphere

Recent developments in the direct-current geoelectrical imaging method

http://www.lithosphere.info/papers/2006-Tecto-Art-TC1-small.pdf

Global 1°×1° thermal model TC1 for the continental lithosphere: Implications for lithosphere secular evolution

George V. Keller

Papers

Geosounding principles, 1. resistivity sounding measurements

Principles of induced polarization for geophysical exploration

Geoelectric and geothermal Studies

Semi-conducting ore minerals