You need JavaScript to view this

Geophysical aspects of vertical streamer seismic data

Abstract

Vertical cable acquisition is performed by deploying a certain number of vertical hydrophone arrays in the water column, and subsequently shooting a source point on top of it. The advantage of this particular geometry is that gives a data set with all azimuths included. Therefore a more complete 3-D velocity model can be derived. In this paper there are presented some results from the Fuji survey in the Gulf of Mexico. Based on these results, improved geometries and review recommendations for future surveys are discussed. 7 figs.
Authors:
Publication Date:
Dec 31, 1998
Product Type:
Conference
Report Number:
NEI-NO-995; CONF-9803138-
Reference Number:
SCA: 150301; PA: NW-99:005011; EDB-99:023513; SN: 99002047423
Resource Relation:
Conference: 1998 geophysical seminar on integrated geophysical techniques in seismic interpretation, Kristiansand (Norway), 9-11 Mar 1998; Other Information: PBD: 1998; Related Information: Is Part Of Integrated geophysical techniques in seismic interpretation: Abstracts; PB: 128 p.
Subject:
15 GEOTHERMAL ENERGY; SEISMIC SURVEYS; MARINE SURVEYS; SEISMIC DETECTORS; SEISMIC SOURCES; DESIGN
OSTI ID:
315250
Research Organizations:
Norsk petroleumsforening, Oslo (Norway)
Country of Origin:
Norway
Language:
English
Other Identifying Numbers:
Other: ON: DE99721549; TRN: NO9905011
Availability:
OSTI as DE99721549
Submitting Site:
NW
Size:
pp. 21.1-21.10
Announcement Date:

Citation Formats

Sognnes, Walter. Geophysical aspects of vertical streamer seismic data. Norway: N. p., 1998. Web.
Sognnes, Walter. Geophysical aspects of vertical streamer seismic data. Norway.
Sognnes, Walter. 1998. "Geophysical aspects of vertical streamer seismic data." Norway.
@misc{etde_315250,
title = {Geophysical aspects of vertical streamer seismic data}
author = {Sognnes, Walter}
abstractNote = {Vertical cable acquisition is performed by deploying a certain number of vertical hydrophone arrays in the water column, and subsequently shooting a source point on top of it. The advantage of this particular geometry is that gives a data set with all azimuths included. Therefore a more complete 3-D velocity model can be derived. In this paper there are presented some results from the Fuji survey in the Gulf of Mexico. Based on these results, improved geometries and review recommendations for future surveys are discussed. 7 figs.}
place = {Norway}
year = {1998}
month = {Dec}
}