Please use this identifier to cite or link to this item: http://ir.library.ui.edu.ng/handle/123456789/1138
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dc.contributor.authorOlowofela, J. A.-
dc.contributor.authorKamiyole, I. C.-
dc.contributor.authorAdegoke, J. A.-
dc.date.accessioned2018-10-08T14:06:18Z-
dc.date.available2018-10-08T14:06:18Z-
dc.date.issued2004-
dc.identifier.issn1742-2131-
dc.identifier.otherJournal of Geophysics and Engineering 1, pp. 234-239-
dc.identifier.otherui_art_olowofela_effects_2004-
dc.identifier.urihttp://ir.library.ui.edu.ng/handle/123456789/1138-
dc.description.abstract"Wave velocities in sandstones are greatly influenced by porosity and clay contents. We formulated new empirical relations for the velocities Vp and Vs in these media which take into account the porosity and clay contents. These relations are Vp=5.57 - 6.47ø - 2.27C1 ø and Vx=3.41 - 4.44ø - 2.23C1 ø, and can be used to compute velocitiesfor various porosities and clay contents. The result compare favourably with those of other works. "en_US
dc.language.isoenen_US
dc.publisherNanjing Institute of Geophysical Prospectingen_US
dc.titleEffects of clay content and porosity on wave velocities in unconsolidated media wing empirical relationsen_US
dc.typeArticleen_US
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