The natural electric field dynamic characters of fracture water in fault
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Abstract
The radial flow of fracture water in faults is comparatively concentrated and can be regarded as a kinetic conductor. The obvious dynamic responses are formed in faint natural electromagnetic field by the flowing groundwater. Its unstable flowing will bring complicated and time-dependent electromagnetic induction on time and space. These dynamic responses are not only related with its depth and hydraulic gradient, but also closely related with observation frequency.
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