Velocity model and static corrections used by N. Cuenot to locate seismic events acquired from the downhole and surface network - Soultz-sous-Forêts 2000 Stimulation
Description
Velocity models described in Nicolas Cuenot's Thesis, used to calculate location of microseismic events from the surface and the downhole network during 2000 stimulation. A first initial model was derived from sonic logs and calibration shots in the well GPK1 and used to perform a preliminary location of hypocenters. The initial model was refined into the final velocity model. The catalogue from Cuenot was obtained by applying the static station corrections with the final velocity model.
The catalogue of events located during 2000 stimulation using both the surface and 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
Location
Temporal coverage
2000
Subjects
Keywords
How to cite
Cuenot, N. 2009. « Réponse du granite fracturé de Soultz-sous-Forêts à des injections massives de fluide: Analyse de la microsismicité induite et du régime de contraintes ». PhD Thesis.
License
Except where otherwise noted, content for this ressource is licensed under a Creative Commons Attribution 4.0 International license.
Ressource last modified on July 1, 2026