Article: Data on geophysics discussed by researchers at University of Idaho.

"Fault hydrology is a topic of scientific and practical importance but considerable uncertainty exists regarding the nature of structural controls on fluid flow. Here we use seismic reflection and time-domain electromagnetic data to develop a three-dimensional model of hydraulic architecture in a predominantly dip-slip normal fault system and we predict the architectural elements based on subsurface fluid flow patterns inferred from near-surface temperature measurements," investigators in the United States report.

"Our observations indicate the presence of high-permeability flow paths parallel to fault planes in poorly-lithified sediments. These results are best ...

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