Abstract
S-wave velocity models are usually poorly constrained in newly developed areas for geothermal heating exploration. Nevertheless, an S-wave model is needed for accurate location of sources of induced seismicity from sparse seismic arrays. We apply seismic noise interferometry to obtain surface waves between receivers and invert the surface waves to determine S-wave velocity structure below an array. We show an application to a sparse array in urban environment in the west of the Netherlands, where significantly low S-wave velocities indicate highly saturated and not very well consolidated sediments.
| Original language | English |
|---|---|
| Title of host publication | 83rd EAGE Conference and Exhibition 2022 |
| Publisher | European Association of Geoscientists and Engineers, EAGE |
| Pages | 1338-1342 |
| Number of pages | 5 |
| ISBN (Electronic) | 9781713859314 |
| State | Published - 2022 |
| Event | 83rd EAGE Conference and Exhibition 2022 - Madrid, Virtual, Spain Duration: 6 Jun 2022 → 9 Jun 2022 |
Publication series
| Name | 83rd EAGE Conference and Exhibition 2022 |
|---|---|
| Volume | 2 |
Conference
| Conference | 83rd EAGE Conference and Exhibition 2022 |
|---|---|
| Country/Territory | Spain |
| City | Madrid, Virtual |
| Period | 6/06/22 → 9/06/22 |
Bibliographical note
Publisher Copyright:Copyright© (2022) by the European Association of Geoscientists & Engineers (EAGE). All rights reserved.
ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
