1887

Abstract

The seismic method attempts to image the subsurface architecture and has been able to significantly contribute to detect<br>areal and vertical changes in rock properties. This work presents a seismic imaging study of channel objects generated<br>using the boolean technique. Three channels having different thicknesses were simulated, using the same width,<br>sinuosity and direction. A velocity model was constructed in order to allow seismic contrasts between the interior of<br>channels and the embedding rock. To examine the seismic response for different channel thicknesses, a 3D ray tracing<br>with a normal incident point survey was performed. The three channels were resolved and the way the seismic could<br>image them was studied.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.215.sbgf189
1999-08-15
2024-04-19
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.215.sbgf189
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