The 15 April 2015
Most large tsunamis are generated by earthquakes on offshore plate boundary megathrusts. The primary factors influencing tsunami excitation are the seismic moment, faulting geometry, and depth of the faulting. Efforts to provide rapid tsunami warning have emphasized seismic and geodetic methods for quickly determining the event size and faulting geometry. It remains difficult to evaluate the updip extent of rupture, which has significant impact on tsunami excitation. Teleseismic
- Award ID(s):
- 1802364
- NSF-PAR ID:
- 10455667
- Publisher / Repository:
- DOI PREFIX: 10.1029
- Date Published:
- Journal Name:
- Journal of Geophysical Research: Solid Earth
- Volume:
- 124
- Issue:
- 10
- ISSN:
- 2169-9313
- Page Range / eLocation ID:
- p. 10583-10609
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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