An illustration of VSP* efficiency to design a geothermal well while - - PowerPoint PPT Presentation

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An illustration of VSP* efficiency to design a geothermal well while - - PowerPoint PPT Presentation

An illustration of VSP* efficiency to design a geothermal well while drilling *Vertical Seismic Profiling Joachim PLACE Charles NAVILLE Edouard Le Garzic Yves Geraud Marc Diraison ENGINE Workshop 4, Reykjavik, 1-5 July 2007 Summary The


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An illustration of VSP* efficiency to design a geothermal well while drilling

Joachim PLACE Charles NAVILLE Edouard Le Garzic Yves Geraud Marc Diraison

ENGINE Workshop 4, Reykjavik, 1-5 July 2007 *Vertical Seismic Profiling

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Summary

  • The interest of VSP
  • After preprocessing
  • After isotropic 3C processing
  • Conclusion
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Why VSP ?

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What is a VSP ?

Vertical Seismic Profiling

  • Zero-offset VSP
  • Offset VSP
  • 1. Velocity survey
  • 2. Structural investigation (after isotropic

processing)

TOOL : 3 orthogonal geophones "3C" 1 hydrophone "4C"

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The VSP surveys in GPK1

1988 1 zero offset VSP + check shots 3 offset VSPs 1 EW-NS walkaway 1993 VSP survey in GPK1 and EPS1 before and after massive fluid injection in GPK1

Data only on paper Data on magnetic tapes

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Summary

  • The interest of VSP
  • After preprocessing
  • After isotropic 3C processing
  • Conclusion
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Example of structural investigation from preprocessed data (1988)

Data only on paper Data on magnetic tapes

Distance D estimation from :

  • Curvature
  • Travel time
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Example of structural investigation from preprocessed data (1988)

The results indicate a distance D of 300 m The diffraction is produced by a major fault affecting the well vicinity Thus, the precise position of the well can be derived from preprocessed data

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Summary

  • The interest of VSP
  • After preprocessing
  • After isotropic 3C processing
  • Conclusion
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Isotropic 3C data processing

Examples of pre-processed data (1999)

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Isotropic 3C data processing

Applied by VSfusion

1. Isotropic upgoing/downgoing separation 2. Single operator deconvolution of the three components

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Most interesting results

Zero offset VSP Offset VSP Arrivals 1 & 2 correspond to well known permeable faults

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P-S reflection

Descartes' law

Thus:

S P

V i V i

2 1

sin sin 32 60 sin 5780 3545 sin sin sin

1 1 1 2 1 2

i V V i

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Most interesting results

Zero offset VSP Offset VSP Arrivals 1 & 2 correspond to well known permeable faults

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Event 3

In total contradiction with Descartes' law !!

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FINAL IMAGE

(from 2D depth migration on Z component)

1. Dip value of the faults 2. Horizontal distance between the well and structures 3. Discover structures which are not drilled

East

Agreement with borehole imagery Deepening/deviation of the well

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Conclusion

VSP is efficient for a structural investigation several hundreds of meters away from a well Design of the deepening/deviation, OR a second geothermal well A preliminary structural investigation can be performed only from preprocessed data !

BUT : processing time are still too long…

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Conclusion

Proposed investigation flow chart : On the long view : Seismic While Drilling

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Example of structural investigation from preprocessed data

Curvature Travel time