Borehole Electroseismic Measurements In Dolomite: Identifying Fractures And Permeable Zones
Name
1998.8 Mikhailov_Toksoz.pdf
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503.93 KB
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Adobe PDF
Checksum (MD5)
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Author(s)
Mikhailov, Oleg V.
Toksoz, M. Nafi
Date Issued
1998
Publisher
Massachusetts Institute of Technology. Earth Resources Laboratory
Series/Report no.
Earth Resources Laboratory Industry Consortia Annual Report;1998-08
Abstract
Measuring the electrical field induced by a borehole Stoneley wave is a new method for
characterizing a rock formation around a borehole. Our field measurements demonstrate
that the Stoneley-wave-induced electrical field can be detected in sedimentary rocks
(dolomite in our experiment), and that the amplitude of this electroseismic phenomenon
can be used to detect isolated fractures and permeable zones.
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