Open Access. Powered by Scholars. Published by Universities.®
- Discipline
- Keyword
-
- Ambient Noise Tomography (1)
- Antarctica (1)
- Chile (1)
- Crust and Uppermost Mantle (1)
- Earthquake hazards (1)
-
- Earthquake; GNSS; tsunami (1)
- Gamburtsev Mountains (1)
- Kinematics of crustal and mantle deformation (1)
- Maule (1)
- Paleoearthquakes (1)
- Plate motions (1)
- Seismicity and tectonics (1)
- Seismology (1)
- Seismotectonics (1)
- Space geodetic surveys (1)
- Transantarctic Mountains (1)
- Tsunami Models (1)
- Tsunami deposits (1)
- Tsunami estimation; real-time GNSS; early warning (1)
- Valdivia (1)
- Publication Type
Articles 1 - 5 of 5
Full-Text Articles in Geophysics and Seismology
The Crust And Upper Mantle Structure Of Central And West Antarctica From Bayesian Inversion Of Rayleigh Wave And Receiver Functions, Weisen Shen, Audrey D. Huerta, J. Paul Winberry
The Crust And Upper Mantle Structure Of Central And West Antarctica From Bayesian Inversion Of Rayleigh Wave And Receiver Functions, Weisen Shen, Audrey D. Huerta, J. Paul Winberry
All Faculty Scholarship for the College of the Sciences
We construct a new seismic model for central and West Antarctica by jointly inverting Rayleigh wave phase and group velocities along with P wave receiver functions. Ambient noise tomography exploiting data from more than 200 seismic stations deployed over the past 18 years is used to construct Rayleigh wave phase and group velocity dispersion maps. Comparison between the ambient noise phase velocity maps with those constructed using teleseismic earthquakes confirms the accuracy of both results. These maps, together with P receiver function waveforms, are used to construct a new 3-D shear velocity (Vs) model for the crust and uppermost mantle …
On The Interaction Of The North Andes Plate With The Caribbean And South American Plates In Northwestern South America From Gps Geodesy And Seismic Data, Omar J. Pérez, Steven G. Wesnousky, Roberto De La Rosa, Julio Márquez, Redescal Uzcátegui, Christian Quintero, Luis Liberal, Héctor Mora-Páez, Walter Szeliga
On The Interaction Of The North Andes Plate With The Caribbean And South American Plates In Northwestern South America From Gps Geodesy And Seismic Data, Omar J. Pérez, Steven G. Wesnousky, Roberto De La Rosa, Julio Márquez, Redescal Uzcátegui, Christian Quintero, Luis Liberal, Héctor Mora-Páez, Walter Szeliga
All Faculty Scholarship for the College of the Sciences
We examine the hypocentral distribution of seismicity and a series of geodetic velocity vectors obtained from Global Positioning System observations between 1994 and 2015 both offshore and mainland northwestern South America (66°W–77°W; 8°N–14°N). Our analysis, that includes a kinematic block modelling, shows that east of the Caribbean–South American–North Andes plates’ triple junction at ∼68°W; 10.7°N, right-lateral easterly oriented shear motion (∼19.6 ± 2.0 mm yr−1) between the Caribbean and South America plates is split along two easterly striking, right-lateral strike-slip subparallel fault zones: the San Sebastián fault that runs off-shore the Venezuelan coast and slips about 17.0±0.5mm …
Assessing The Use Of Tsunami Simulations As A Tool To Predict Source Magnitudes And Locations Of Paleoearthquakes In Chile, Rebeca Isabel Becerra
Assessing The Use Of Tsunami Simulations As A Tool To Predict Source Magnitudes And Locations Of Paleoearthquakes In Chile, Rebeca Isabel Becerra
All Master's Theses
A long-term goal of paleotsunami studies is the ability to predict paleoearthquake parameters based on tsunami deposits found on land. Chile provides an exemplary location for testing methods of making these predictions because the historical record includes 41 major earthquakes as far back as 1562 AD, and there are many known paleotsunami deposits throughout the region. Using these records as a comparison tool, I evaluated simulated tsunami wave heights and inundation extent with the tsunami model GeoClaw for nine hypothetical tsunamigenic large earthquakes (Mw 8.6, 8.8, and 9.0) in south-central Chile with epicenters at -35.1º, -38.8º, and -42.9º. As …
Tsunami Excitation Estimation From Real-Time Gnss, Catherine Jeffries
Tsunami Excitation Estimation From Real-Time Gnss, Catherine Jeffries
All Master's Theses
Tsunami early warning systems currently comprise modeling of observations from the global seismic network, deep-ocean DART buoys, and a global distribution of tide gauges. While these tools work well for tsunamis traveling teleseismic distances, saturation of seismic magnitude estimation in the near field can result in significant underestimation of tsunami excitation for local warning (Wang et al., 2012). Moreover, DART buoy and tide gauge observations cannot be used to rectify the underestimation in the available time, typically 10-20 minutes, before local runup occurs. Real-time GNSS measurements of coseismic offsets may be used to estimate finite faulting within 1-2 minutes and, …
Slip Estimation From Real-Time Gps In Cascadia, Jesse Senko
Slip Estimation From Real-Time Gps In Cascadia, Jesse Senko
All Master's Theses
Current systems for rapidly characterizing earthquakes are based on seismic, teleseismic, and Deep-ocean Assessment and Reporting of Tsunami (DART) buoy data. These systems have significant limitations that hinder them from making rapid and accurate assessments of large earthquakes used for local tsunami warnings where run-up can occur minutes after the earthquake. Seismic and teleseismic networks saturate around Mw 7.0. Tsunami waves take tens of minutes to reach the buoys, so rapid assessment is impossible. GPS overcomes these limitations for large earthquakes. GPS does not saturate, and the offsets being detected occur very quickly after an earthquake. This thesis develops …