Travel Time Changes in the Groningen Gas Reservoir by Train Noise Interferometry of Borehole Data

References

1. Behm, M.
   [2017]. Feasibility of borehole ambient noise interferometry for permanent reservoir monitoring. Geophysical Prospecting, 65(2), 563–580.
   [Google Scholar]
2. Cannon, M. & Kole, P.
   [2018]. The first year of distributed strain sensing (DSS) monitoring in the Groningen gas field. NAM report.
   [Google Scholar]
3. Grechka, V. & Zhao, Y.
   [2012]. Microseismic interferometry. The Leading Edge, 31(12), 1478–1483.
   [Google Scholar]
4. Hatchell, P. & Bourne, S.
   [2005]. Rocks under strain: strain-induced time-lapse time shifts are observed for depleting reservoirs. The Leading Edge, 24, 1222–1225.
   [Google Scholar]
5. MacBeth, C., Mangriotis, M.-D. & Amini, H.
   [2019]. Review paper: Post stack 4D seismic time-shifts: Interpretation and evaluation. Geophysical Prospecting, 67, 3–31.
   [Google Scholar]
6. Miyazawa, M., Snieder, R. & Venkataraman, A.
   [2008]. Application of seismic interferometry to extract P-and S-wave propagation and observation of shear-wave splitting from noise data at Cold Lake, Alberta, Canada. Geophysics, 73(4), D35–D40.
   [Google Scholar]
7. Vaezi, Y. & Van der Baan, M.
   [2015]. Interferometric assessment of clamping quality of borehole geophones. Geophysics, 80(6), WC89–WC98.
   [Google Scholar]
8. Zhou, W. & Paulssen, H.
   [2017]. P and S velocity structure in the Groningen gas reservoir from noise interferometry. Geophysical Research Letters, 44(23), 1–7.
   [Google Scholar]