London 2013, 75th Eage Conference en Exhibition Incorporating SPE Europec 2013
DOI: 10.3997/2214-4609.20130005
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Mitigation of the 3D Cross-line Acquisition Footprint Using Separated Wavefield Imaging of Dual-sensor Streamer Seismic

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Cited by 5 publications
(3 citation statements)
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“…It has been demonstrated that the concept of virtual source imaging (Wapenaar et al, 2010) can be extended to multi-sensor streamer acquisition to utilize sea surface reflected downgoing wavefield energy that provides the missing near-surface information. Recent case studies (e.g., Long et al, 2013 andRønholt et al, 2014), demonstrate how separated wavefield imaging from dualsensor systems can be used to remove acquisition footprints and shallow coverage gaps that are evident if only the primary reflections are used ( Figure 5). The shallow overburden can not only be imaged seamlessly, but also complemented by AVO/AVA analysis facilitated by the virtual source concept.…”
Section: Improving Near-surface Imagingmentioning
confidence: 99%
“…It has been demonstrated that the concept of virtual source imaging (Wapenaar et al, 2010) can be extended to multi-sensor streamer acquisition to utilize sea surface reflected downgoing wavefield energy that provides the missing near-surface information. Recent case studies (e.g., Long et al, 2013 andRønholt et al, 2014), demonstrate how separated wavefield imaging from dualsensor systems can be used to remove acquisition footprints and shallow coverage gaps that are evident if only the primary reflections are used ( Figure 5). The shallow overburden can not only be imaged seamlessly, but also complemented by AVO/AVA analysis facilitated by the virtual source concept.…”
Section: Improving Near-surface Imagingmentioning
confidence: 99%
“…It is this difference in polarity that facilitates proper wavefield separation. Figure 1 shows a shallow imaging example from a 3D dual-sensor towed streamer survey over the Tenggol Arch area in offshore Peninsular Malaysia (Long et al, 2013). Water depth is approximately 70 m. This survey was acquired in 2011 using a 12 x 4050 m dual-sensor streamer spread with 75 m separation and 15 m streamer depth.…”
Section: Seismic Imaging Of Shallow Anomalies With Dual-sensor Towed mentioning
confidence: 99%
“…By utilising broad-band dual sensor seismic data it is now possible to use the complete wave-field to image the overburden in great detail in complex geological settings. For example, Long et al (2013) and Rønholt et al (2014) presented shallow water case studies that illustrated how the free surface multiple reflections, i. e. down-going wave-field can be used to image the overburden, and remove the acquisition footprint that is evident if only the primary reflections are used. The fact that the 3D seismic acquisition footprint can be effectively eliminated, and that the shallow sub-surface can be imaged in great detail, opens up the possibility that exploration seismic data can be used to identify and interpret shallow anomalies with confidence.…”
Section: Introductionmentioning
confidence: 99%