VSP Flashcards

1
Q

What is a VSP ?

A

VSP is both a log and seismic image tool

the geophone is lowered into the borehole and then raised up gradually

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2
Q

Why are VSPs useful ?

A
  • 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.

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3
Q

What are the components of VSPs? (4)

A

1- seismic source array
2- wireline
3- downhold receiver array
4- recording/wireline truck

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4
Q

Types of VSPs (5)

A
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
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5
Q

Zero Offset VSP

A

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

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6
Q

walkaway VSP

A

several regularly offset sources from the well head.
1- determine AVO behaviour
2- create 2D reflectivity image

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7
Q

multi-offset VSP

A

several sources at various offsets

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8
Q

multi-azimuth VSP

A

several sources in different directions

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9
Q

cross-well VSP

A

need 2 adjacent wells

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10
Q

Composite plot

A
  • 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).
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11
Q

3D VSP

A

full areal set of shots on the surface.

can be shot in conjunction with 3D surface seismic survey

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12
Q

Objective using 3D VSP

A

make a full 3D image of the subsurface using VSP and surface seismic

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13
Q

downgoing

A

last leg of travel path is “down” toward the geophone

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14
Q

upgoing

A

last leg of travel path is “up” toward the grophone

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15
Q

VSP Processing Steps

A

Deconvolution
Stack
Filter
Scale

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