Thesis (Ph.D.) University of Alaska Fairbanks, 2018This thesis presents: (1) a set of earthquake source mechanism catalogs for Alaska and (2) a threedimensional seismic velocity model of Alaska. The improved earthquake sources are used within the velocity model for generating synthetic seismograms, which are then compared with recorded seismograms to assess the quality of the velocity model. An earthquake source mechanism can be modeled as a moment tensor, which is a 3 × 3 symmetric matrix. We estimate the moment tensor for earthquakes by comparing observed waveforms (body waves and surface waves) with synthetic waveforms computed in a layered model. The improved moment tensor solutions are obtained by utilizing both the body waves and surface waves at as many broadband stations as possible. Further improvement in the inversion technique is obtained by (1) implementation of L1 norm in waveform misfit function and (2) inclusion of first-motion polarity misfit in the misfit function. We also demonstrate a probabilistic approach for quantifying the uncertainty in a moment tensor solution. Moment tensors can be used for understanding the tectonics of a region. In the Cook Inlet and Susitna region, west of Anchorage, we determined moment tensor solutions for small-tointermediate magnitude (M ≥ 2.5) crustal earthquakes. Analyzing these small earthquakes required us to modify the misfit function to include first-motion polarity measurements, in addition to waveform differences. The study was complemented with the probabilistic hypocenter estimation of large historical earthquakes (Mw ≥ 5.8) to assess their likelihood of origin as crustal, intraslab, or subduction interface. The predominance of thrust faulting mechanisms for crustal earthquakes indicate a compressive regime within the crust of south-central Alaska. Wavefield simulations are performed in three regions of Alaska: the southern Alaska region of subduction, the eastern Alaska region with the accreting Yakutat microplate, and the interior Alaska region containing predominantly strike-slip faulting, including the Minto Flats fault zone. Our three-dimensional seismic velocity model of Alaska is an interpolated body-wave arrival time model from a previous study, embedded with major sedimentary basins (Cook Inlet, Susitna, Nenana), and with a minimum shear wave velocity threshold of 1000 m/s. Our comparisons between data and synthetics quantify the misfit that arises from different parts of each model. Furtherwork is needed to comprehensively document the regions within each model that give rise to the observed misfit. This would be a step toward performing an iterative adjoint tomographic inversion in Alaska.National Science Foundation, Alaska Earthquake Center, U.S. Geological Survey Earthquake Hazards Program, Air Force Research Laborator
