Velocity model and station corrections used by B. Dyer to locate seismic events recorded by the downhole and the surface network - Soultz-sous-Forêts 2000 Stimulation
Description
Velocity model and static station corrections described in B. Dyer's report [see part 1.5.3 Velocity model and station corrections].
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. Semore Seismic report for Socomine).
The catalogue of events located by B. Dyer using the downhole network is available here.
The catalogue of events located by B. Dyer using the surface 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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Dyer, B. 2001. “Soultz GPK2 Stimulation June/July 2000. Seismic Monitoring Report.” Semore Seismic report for Socomine. IsReferencedBy
Report
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Stakeholders
Rights Holder(s)
GEIE - Exploitation Minière de la Chaleur
Location
Temporal coverage
2000
Subjects
Keywords
How to cite
Dyer, B. 2001. “Soultz GPK2 Stimulation June/July 2000. Seismic Monitoring Report.” Semore Seismic report 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