ASU Electronic Theses and Dissertations
This collection includes most of the ASU Theses and Dissertations from 2011 to present. ASU Theses and Dissertations are available in downloadable PDF format; however, a small percentage of items are under embargo. Information about the dissertations/theses includes degree information, committee members, an abstract, supporting data or media.
In addition to the electronic theses found in the ASU Digital Repository, ASU Theses and Dissertations can be found in the ASU Library Catalog.
Dissertations and Theses granted by Arizona State University are archived and made available through a joint effort of the ASU Graduate College and the ASU Libraries. For more information or questions about this collection contact or visit the Digital Repository ETD Library Guide or contact the ASU Graduate College at firstname.lastname@example.org.
- 3 English
- 3 Public
- 2 Geophysics
- 2 InSAR
- 2 Remote sensing
- 1 Active fault in Java volcanic arc
- 1 Active tectonics in humid environment
- 1 Crustal deformation in Subduction Zone
- 1 Earthquake Hazard
- 1 Earthquake geology of a volcanic arc
- 1 Fault Creep
- 1 Geological engineering
- 1 Geomorphology
- 1 Indonesia
- 1 Induced Seismicity
- 1 Inversion Theory
- 1 Magmatic Source Modeling
- 1 Northeast Japan Subduction Zone
- 1 Paleoseismology
- 1 Poroelasticity
- 1 San Andreas Fault
- 1 Slow Slip Events
- 1 Tectonic geomorphology
- 1 Volcano Deformation
The movement between tectonic plates is accommodated through brittle (elastic) displacement on the plate boundary faults and ductile permanent deformation on the fault borderland. The elastic displacement along the fault can occur in the form of either large seismic events or aseismic slip, known as fault creep. Fault creep mainly occurs at the deep ductile portion of the crust, where the temperature is high. Nonetheless, aseismic creep can also occur on the shallow brittle portion of the fault segments that are characterized by frictionally weak material, elevated pore fluid pressure, or geometrical complexity. Creeping segments are assumed to safely release …
- Khoshmanesh, Mostafa, Shirzaei, Manoochehr, Arrowsmith, Ramon, et al.
- Created Date
The dynamic Earth involves feedbacks between the solid crust and both natural and anthropogenic fluid flows. Fluid-rock interactions drive many Earth phenomena, including volcanic unrest, seismic activities, and hydrological responses. Mitigating the hazards associated with these activities requires fundamental understanding of the underlying physical processes. Therefore, geophysical monitoring in combination with modeling provides valuable tools, suitable for hazard mitigation and risk management efforts. Magmatic activities and induced seismicity linked to fluid injection are two natural and anthropogenic processes discussed in this dissertation. Successful forecasting of the timing, style, and intensity of a volcanic eruption is made possible by improved understanding …
- Zhai, Guang, Shirzaei, Manoochehr, Garnero, Edward, et al.
- Created Date
Shallow earthquakes in the upper part of the overriding plate of subduction zones can be devastating due to their proximity to population centers despite the smaller rupture extents than commonly occur on subduction megathrusts that produce the largest earthquakes. Damaging effects can be greater in volcanic arcs like Java because ground shaking is amplified by surficial deposits of uncompacted volcaniclastic sediments. Identifying the upper-plate structures and their potential hazards is key for minimizing the dangers they pose. In particular, the knowledge of the regional stress field and deformation pattern in this region will help us to better understand how subduction …
- Marliyani, Gayatri Indah, Arrowsmith, J Ramon, Clarke, Amanda B, et al.
- Created Date