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Unformatted text preview: analysis. Wenner: h=a/2 Schlumberger: h=L/3 Dipole Dipole: h=n a Pseudo-Sections • Can sometimes be used to qualitatively assess geology • Warning : Can also prove to be very difficult to interpret directly, with different arrays yielding very different results....
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This note was uploaded on 01/07/2012 for the course PHYSICS 384 taught by Professor Wei during the Spring '09 term at SUNY Stony Brook.
- Spring '09