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...
| Main Authors: | , |
|---|---|
| Format: | Journal Article |
| Published: |
AMERICAN GEOPHYSICAL UNION
2006
|
| Online Access: | http://hdl.handle.net/20.500.11937/22069 |