VSP Flashcards
What is a VSP ?
VSP is both a log and seismic image tool
the geophone is lowered into the borehole and then raised up gradually
Why are VSPs useful ?
- VSPs are useful because they provide in situ rock properties in depth (seismic velocity, impedance, anisotropy and attentuation)
- assist in understanding seismic wave propogation (source signature, multiples and conversions)
You match the VSP with surface seismic to identify multiples in surface seismic data.
What are the components of VSPs? (4)
1- seismic source array
2- wireline
3- downhold receiver array
4- recording/wireline truck
Types of VSPs (5)
List and Draw 1- Zero-offset VSP 2- walkaway VSP 3- multi-offset VSP 4- multi-azimuth VSP 5- cross-well VSP 6- 3D VSPs
Zero Offset VSP
single source position used within several tens of metres of the borehole.
1- provide seismic time-to-depth relationship
2- interval velocities in depth,
3- normal incidence
walkaway VSP
several regularly offset sources from the well head.
1- determine AVO behaviour
2- create 2D reflectivity image
multi-offset VSP
several sources at various offsets
multi-azimuth VSP
several sources in different directions
cross-well VSP
need 2 adjacent wells
Composite plot
- well logs (sonic and gamma log in depth)
- synthetic seismograms
- VSP data (in TWT on teh vertical axis. Offset VSP yields an offset image both for P waves and converted PS waves
- surface seismic(VSP images can be correlated and integrated into the interpretation).
3D VSP
full areal set of shots on the surface.
can be shot in conjunction with 3D surface seismic survey
Objective using 3D VSP
make a full 3D image of the subsurface using VSP and surface seismic
downgoing
last leg of travel path is “down” toward the geophone
upgoing
last leg of travel path is “up” toward the grophone
VSP Processing Steps
Deconvolution
Stack
Filter
Scale