Velocity model and static corrections used by B. Dyer to locate seismic events acquired from the downhole network - Soultz-sous-Forêts 2000 Stimulation
Description
Velocity model and static station corrections described in B.Dyer's report. The velocity model was derived from a combination of the GPK1 check shot survey velocities and the velocity gradient interpreted from the GPK1 sonic logs. The station corrections were refined from initial station corrections by removing any bias between the model traveltimes and the picked P and S wave arrivals (Dyer, B. 2001. Soultz GPK2 Stimulation June/July 2000. Seismic Monitoring Report.).
The catalogue of events located during 2000 stimulation using the downhole network is available here.
This resource is available for download upon request.
This ressource is in following collection(s)
https://doi.org/10.25577/SSFS2000
Associated ressources
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How to cite: Dyer, B. 2001. “Soultz GPK2 Stimulation June/July 2000. Seismic Monitoring Report.” Semore Seismic for Socomine. IsReferencedBy
ConferencePaper
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Dyer, B., R. Baria, et S. Michelet. 2004. « Soultz GPK3 stimulation and GPK3-GPK2 circulation May to July 2003 - Seismic monitoring report ». Report n° EEIG 05/2004. Semore Seismic for Socomine. IsReferencedBy
ConferencePaper
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Location
Temporal coverage
2000
Subjects
Keywords
How to cite
Dyer, B. 2001. “Soultz GPK2 Stimulation June/July 2000. Seismic Monitoring Report.” Semore Seismic for Socomine.
License
Except where otherwise noted, content for this ressource is licensed under a Creative Commons Attribution 4.0 International license.
Ressource last modified on May 28, 2026