Vertical seismoelectric profiling in a borehold penetrating glaciofluvial sediments

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Vertical seismoelectric profiling in a borehold penetrating glaciofluvial sediments

Seismoelectric signals have been measured as a function of depth in a borehole penetrating glaciofluvial sands, silts, and glacial till using a broadband surface seismic source, and a downhole electrode array. Transient electric field pulses, with amplitudes of 1 to 4 μV/m accompanied the arrival of...

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Bibliographic Details
Main Authors:	Dupuis, Christian, Butler, K.
Format:	Journal Article
Published:	AMERICAN GEOPHYSICAL UNION 2006
Online Access:	http://hdl.handle.net/20.500.11937/22069

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