ERC Advanced Grant · 2016
If it were possible to place seismometers and seismic vibrators anywhere below the ground in, for example, an induced-earthquake-sensitive area, we could measure the source mechanism of actual earthquakes, monitor the geomechanical state of the area over time, and quantify the ground motion caused by possible future earthquakes. Moreover, we could monitor fluid flow in aquifers, geothermal reservoirs or CO2 storage reservoirs, with unprecedented resolution. Unfortunately, placing seismic instruments anywhere below the ground is not practically feasible. I propose to develop groundbreaking methodology for creating virtual seismic sources (earthquakes or seismic vibrators) and virtual…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.