Time‐lapse monitoring of rock properties with coda wave interferometry

By A. Grêt, Roel Snieder, John A. Scales. 2006

181 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/2d5953887255dd3b3a0dfb1cbca450ebbdfef6bf

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

1. Roel Snieder
2. Kees Wapenaar
3. Evert C. Slob
4. Andrew Curtis
5. M. Heap
6. P. Baud
7. O. Lengliné
8. L. Griffiths

In Ocean Engineering

1. Kees Wapenaar
2. Roel Snieder
3. Andrew Curtis
4. Evert C. Slob
5. M. Heap
6. L. Griffiths
7. J. Schmittbuhl
8. O. Lengliné

Citations in the corpus

• The Theory of Coda Wave Interferometry (2006, background): “, 2001), and in ultrasound experiments (ROBERTS et al., 1992; SNIEDER et al., 2002; GRÊT et al., 2006).”
• Thermal Cracking in Westerly Granite Monitored Using Direct Wave Velocity, Coda Wave Interferometry, and Acoustic Emissions (2018, methodology): “Overall, we find similar values to those of Grêt et al. (2006)— δtt of between 2 × 10 4/°C and 6 × 10 4/°C—when they heated and cooled Elberton Granite to a maximum temperature of 90°C, confirming our approach.”
• Tutorial on seismic interferometry: Part 2 — Underlying theory and new advances (2010, methodology): “(2002) and Grêt et al. (2006) employ the repeatability of acoustic experiments in a method they call coda wave interferometry (here the term “interferometry” is used in the classical sense).”