Now showing items 1-10 of 33
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 ...
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 ...
Interpretation of Southern Georgia coastal plain velocity structure using refraction and wide-angle reflection methods
(Georgia Institute of Technology, 1988-05)
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 ...
AVO limitations near salt structures
(Georgia Institute of Technology, 1992-05)
Temporal change of seismic velocity and site response for different scales and implications for nonlinearity
(Georgia Institute of Technology, 2007-07-10)
This thesis consists of two major parts. In the first part, I monitor the temporal change of S-wave velocity in shallow soil layers using seismic data collected in an experiment at Panola Mt. Atlanta, GA, 2006. I use the ...
Collaborative Research: Seismic and Geologic Study of Gulf of California Rifting and Magmatism
(Georgia Institute of Technology, 2002-04-01)
Investigation of SV to P wave amplitude ratio for determining focal mechanism
(Georgia Institute of Technology, 1982-08)
Influence of focal depth on the displacement spectra of earthquakes
(Georgia Institute of Technology, 1983-12)
Modeling of seismic coda, with application to attenuation and scattering in southeastern Tennessee
(Georgia Institute of Technology, 1988-08)