ToC2ME Velocity Model
Nadine Igonin · Zenodo (CERN European Organization for Nuclear Research) · 2021
Velocity model used for locating microseismic events for the ToC2ME dataset (.mat file). P-wave velocity comes from a blocked well log close to where the dataset was acquired. The S-wave velocity was obtained from the P-wave velocity, using layer-specific vp/vs ratios obtained from co-located 3D/3C seismic data. Depth starts from the surface (set to 0m), with a TVD reference elevation of 898.5 m above sea level. For more information see https://github.com/ToC2ME