Velocity model used by N. Cuenot to locate seismic events with a tomographic inversion method - Soultz-sous-Forêts 2000 Stimulation
Description
Velocity model described in the PhD thesis of N. Cuenot, used to calculate location of microseismic events of his second catalogue of the 2000 episode at Soultz-sous-Forêts.
N. Cuenot used a local tomographic method to get more precise locations for his second catalogue as part of his PhD. The distributed velocity model is the input 1-D layered model required for the tomographic calculations.
The second catalogue of events of the 2000 episode calculated by N. Cuenot using tomographic inversion 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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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, Université de Strasbourg. IsReferencedBy
JournalArticle
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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, Université de Strasbourg.
License
Except where otherwise noted, content for this ressource is licensed under a Creative Commons Attribution 4.0 International license.
Ressource last modified on June 15, 2026