Abstract
The effect of near-source velocity structure on the recovery of the isotropic component in moment tensor inversions is explored using a finite-difference method. Synthetic data generated using a 3D Long Valley Caldera (LVC) velocity model (Vp +/- 20%) were inverted for the full moment tensor using a linear time-domain scheme utilizing Green's functions calculated from 1D models. While inversions of synthetic data with input isotropic components recovered isotropic components with 95% significance according to an F-test relative to deviatoric inversions (isotropic component constrained to zero), inversions of synthetic data with no input isotropic component recovered only nominal isotropic components with less than 75% significance. This study demonstrates near-source structure does not appear to falsely produce significant isotropic components of moment tensor inversions in the passband typically employed by regional inversion methods.
| Original language | English |
|---|---|
| Pages (from-to) | 1815-1818 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 28 |
| Issue number | 9 |
| DOIs | |
| Publication status | Published - 1 May 2001 |
| Externally published | Yes |