| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9527098 | Tectonophysics | 2005 | 24 Pages |
Abstract
Furthermore, two distinct phases of energy releases, corresponding to two sub-events of the earthquake have been identified on the 'SH wave' records. The sub-events, which represent asperities in the fault process, are separated in time by about 6 s and 20 km in space. The fault plane solution, seismic moment and stress drop of these asperities have also been obtained.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Dinesh Kumar, Irene Sarkar, V. Sriram, K.N. Khattri,