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dc.contributor.authorKnapp, Ralph W.
dc.contributor.authorSteeples, Don W.
dc.date.accessioned2015-04-02T19:32:50Z
dc.date.available2015-04-02T19:32:50Z
dc.date.issued1986-02-01
dc.identifier.citationKnapp, R.W. & Steeples, D.W. (1986). ”High‐resolution common‐depth‐point reflection profiling:Field acquisition parameter design.” High‐resolution common‐depth‐point reflection profiling:Field acquisition parameter design, 51(2), 283-294. http://www.dx.doi.org/10.1190/1.1442088en_US
dc.identifier.issn0016-8033
dc.identifier.urihttp://hdl.handle.net/1808/17300
dc.descriptionThis is the publisher's version, also available electronically from "http://library.seg.org".en_US
dc.description.abstractThe results of a seismic reflection profiling exercise are strongly dependent upon parameters used in field recording. The choice of parameters is determined by objectives of the survey, available resources, and geologic locality. Some simple modeling and/or a walkaway noise survey are helpful in choice of field parameters. Filtering data before analog‐to‐digital conversion in the field can help overcome limitations in the dynamic range of the seismograph. Source and geophone arrays can be used to a limited extent in high‐resolution surveys to help attenuate ground roll. Proper planting of geophones can be an important factor in obtaining the flattest spectral response. Various seismic energy sources provide the flattest spectral response. Various seismic energy sources provide different spectral character and varying degrees of convenience and cost.en_US
dc.publisherSociety of Exploration Geophysicistsen_US
dc.titleHigh-resolution common depth point seismic reflection profiling: field acquisition parameter designen_US
dc.typeArticle
kusw.kuauthorSteeples, Don W.
kusw.kudepartmentGeologyen_US
dc.identifier.doi10.1190/1.1442088
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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