Source process of complex earthquakes by time-dependent moment tensor analysis
Seismic source complexity, which may be due to fault geometry changes or discrete subevents, is difficult to quantify with conventional moment tensor inversion techniques. The time-dependent moment tensor (TDMT) inversion procedure is an attempt to extract a time varying source from teleseismic P-wa...
| Main Author: | |
|---|---|
| Other Authors: | |
| Language: | en_US |
| Published: |
The University of Arizona.
1996
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10150/282274 |