AZIMUTH CORRECTION FOR DATA RECONSTRUCTION IN THREE-DIMENSIONAL SURFACE-RELATED MULTIPLE PREDICTION
A best fitting trace in seismic data is determined for a desired trace to be reconstructed. An azimuth correction is calculated for the azimuth difference between the best fitting trace and the desired trace. The azimuth correction is applied to the best fitting trace to reconstruct the desired trac...
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creator | HEGGE, ROBERTUS F BARNES, SIMON R VAN BORSELEN, ROALD G AARON, PETER A |
description | A best fitting trace in seismic data is determined for a desired trace to be reconstructed. An azimuth correction is calculated for the azimuth difference between the best fitting trace and the desired trace. The azimuth correction is applied to the best fitting trace to reconstruct the desired trace for 3D surface-related multiple prediction.
Una traza de ajuste óptimo en datos sísmicos es determinada para una traza deseada a reconstruir. Una corrección de azimut se calcula para la diferencia de azimut entre la traza de ajuste óptimo y la traza deseada. La corrección de azimut es aplicada a la traza de ajuste óptimo para reconstruir la traza deseada para predicción de múltiples relacionados con la superficie 3D. |
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Una traza de ajuste óptimo en datos sísmicos es determinada para una traza deseada a reconstruir. Una corrección de azimut se calcula para la diferencia de azimut entre la traza de ajuste óptimo y la traza deseada. La corrección de azimut es aplicada a la traza de ajuste óptimo para reconstruir la traza deseada para predicción de múltiples relacionados con la superficie 3D.</description><language>eng ; spa</language><subject>CALCULATING ; COMPUTING ; COUNTING ; DETECTING MASSES OR OBJECTS ; ELECTRIC DIGITAL DATA PROCESSING ; GEOPHYSICS ; GRAVITATIONAL MEASUREMENTS ; MEASURING ; PHYSICS ; TESTING</subject><creationdate>2011</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://worldwide.espacenet.com/publicationDetails/biblio?FT=D&date=20110719&DB=EPODOC&CC=MX&NR=2011000770A$$EHTML$$P50$$Gepo$$Hfree_for_read</linktohtml><link.rule.ids>230,308,777,882,25545,76296</link.rule.ids><linktorsrc>$$Uhttps://worldwide.espacenet.com/publicationDetails/biblio?FT=D&date=20110719&DB=EPODOC&CC=MX&NR=2011000770A$$EView_record_in_European_Patent_Office$$FView_record_in_$$GEuropean_Patent_Office$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>HEGGE, ROBERTUS F</creatorcontrib><creatorcontrib>BARNES, SIMON R</creatorcontrib><creatorcontrib>VAN BORSELEN, ROALD G</creatorcontrib><creatorcontrib>AARON, PETER A</creatorcontrib><title>AZIMUTH CORRECTION FOR DATA RECONSTRUCTION IN THREE-DIMENSIONAL SURFACE-RELATED MULTIPLE PREDICTION</title><description>A best fitting trace in seismic data is determined for a desired trace to be reconstructed. An azimuth correction is calculated for the azimuth difference between the best fitting trace and the desired trace. The azimuth correction is applied to the best fitting trace to reconstruct the desired trace for 3D surface-related multiple prediction.
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Una traza de ajuste óptimo en datos sísmicos es determinada para una traza deseada a reconstruir. Una corrección de azimut se calcula para la diferencia de azimut entre la traza de ajuste óptimo y la traza deseada. La corrección de azimut es aplicada a la traza de ajuste óptimo para reconstruir la traza deseada para predicción de múltiples relacionados con la superficie 3D.</abstract><oa>free_for_read</oa></addata></record> |
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subjects | CALCULATING COMPUTING COUNTING DETECTING MASSES OR OBJECTS ELECTRIC DIGITAL DATA PROCESSING GEOPHYSICS GRAVITATIONAL MEASUREMENTS MEASURING PHYSICS TESTING |
title | AZIMUTH CORRECTION FOR DATA RECONSTRUCTION IN THREE-DIMENSIONAL SURFACE-RELATED MULTIPLE PREDICTION |
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