1887
PDF

Abstract

Traditionally, towed marine cables measure the seismic wavefield using only pressure sensors<br>(hydrophones). By contrast, in a dual-sensor streamer, independent measurements of the total<br>pressure and particle velocity wavefields are obtained using collocated sensors. These two<br>measurements of the seismic wavefield can be combined in processing to separate the wavefield into<br>up- and down-going components. 2-D case examples have demonstrated that this procedure is both<br>robust and accurate. This concept has now been extended to 3-D acquisition geometries. It has been<br>shown that 3-D dual-sensor streamer acquisition avoids exposure to weather, sea-state and streamer<br>spread control downtime by efficiently towing the entire 3-D streamer spread deep and at one common<br>depth. Removal of the receiver ghost effects simultaneously boosts both low and high frequencies<br>beyond any result achievable with conventional hydrophone-only streamers, and maximizes low<br>frequency signal-to-noise content required for accurate seismic inversion and reservoir description.<br>These applications are illustrated using data examples from a number of 3-D dual-sensor streamer surveys.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.248.349
2010-03-07
2024-04-20
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.248.349
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error