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Statistical techniques for studying seismicity rate changes and magnitude stability in the California Seismicity catalogs
(Georgia Institute of Technology, 1988)
Microseismic data
(Georgia Institute of Technology, 1986)
Continuation of quantitive asperity recognition of subduction zones
(Georgia Institute of Technology, 1986)
Asperity recognition in subduction zones
(Georgia Institute of Technology, 1985)
Systematic study of earthquake triggering using microearthquakes detected by the matched filter technique
(Georgia Institute of Technology, 2015-06-18)
Earthquakes can be promoted or inhibited by surprisingly small stress perturbations, known as earthquake triggering. The stress perturbations can stem from various natural and anthropogenic processes. The most common stress ...
Fault zone imaging and earthquake detection with dense seismic arrays
(Georgia Institute of Technology, 2017-07-13)
Natural earthquakes occur on faults. The relationship between fault zone structures and earthquake behaviors remains one of the most interesting problems in seismology. As an important tool to detect earthquakes and image ...
Postseismic response following the 2012 Mw 7.6 Nicoya, Costa Rica earthquake
(Georgia Institute of Technology, 2019-03-27)
Characterization of the surface deformation related to the 2012 moment magnitude (Mw) 7.6 Nicoya earthquake was undertaken using continuous and campaign Global Positioning System (GPS) observations. This location is uniquely ...
Influence of scattering on Q in the lithosphere
(Georgia Institute of Technology, 1984)
Collaborative Research: Seismic and Geologic Study of Gulf of California Rifting and Magmatism
(Georgia Institute of Technology, 2002-04-01)
Teleseismic P codas : source and receiver envelopes
(Georgia Institute of Technology, 1985)