Borehole Electroseismic Measurements In Dolomite: Identifying Fractures And Permeable Zones

dc.contributor.author	Mikhailov, Oleg V.
dc.contributor.author	Toksoz, M. Nafi
dc.contributor.other	Massachusetts Institute of Technology. Earth Resources Laboratory	en_US
dc.date.accessioned	2012-12-11T16:41:48Z
dc.date.available	2012-12-11T16:41:48Z
dc.date.issued	1998
dc.identifier.uri	http://hdl.handle.net/1721.1/75384
dc.description.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.	en_US
dc.publisher	Massachusetts Institute of Technology. Earth Resources Laboratory	en_US
dc.relation.ispartofseries	Earth Resources Laboratory Industry Consortia Annual Report;1998-08
dc.title	Borehole Electroseismic Measurements In Dolomite: Identifying Fractures And Permeable Zones	en_US
dc.type	Technical Report	en_US
dc.contributor.mitauthor	Mikhailov, Oleg V.
dc.contributor.mitauthor	Toksoz, M. Nafi
dspace.orderedauthors	Mikhailov, Oleg V.; Toksoz, M. Nafi	en_US