Coda wave interferometry during the heating of deep geothermal reservoir rocks

Coda wave interferometry during the heating of deep geothermal reservoir rocks

Abstract Coda wave interferometry (CWI) is a high-resolution technique that aims at tracking small changes in a diffusive medium from the time correlation of seismic waveforms. CWI has been widely used in recent years to monitor the fine-scale evolution of fault zones and more recently of deep reser...

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Bibliographic Details
Main Authors: Jérôme Azzola, Luke Griffiths, Jean Schmittbuhl, Dimitri Zigone, Vincent Magnenet, Frédéric Masson, Michael Heap, Patrick Baud
Format: Article
Language:English
Published: SpringerOpen 2018-10-01
Series:Geothermal Energy
Subjects:
Coda wave interferometry
Westerly Granite
Deep geothermal reservoir
Wave propagation simulation (SPECFEM2D)
Thermo-elastic deformation simulation (Code ASTER)
Online Access:http://link.springer.com/article/10.1186/s40517-018-0107-2

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http://link.springer.com/article/10.1186/s40517-018-0107-2

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