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This book presents investigations on the Earth's seismic structure
using both active-source and natural earthquake records. It
discusses the ground-truth data obtained from the TAiwan Integrated
GEodynamics Research (TAIGER) active-source experiments that
provides excellent and unique insights into the shallow crustal
structures beneath Taiwan. It also explores the full-wave
sensitivity kernels, which account for the effects of all possible
wave interferences involved in shear-wave splitting and therefore
loosen the restrictions on source-receiver geometry amenable to
shear-wave splitting analysis. Moreover, it describes the 3D
Frechet kernels, which enable us to resolve the vertical and
lateral variations in seismic anisotropy and obtain 3D images of
the Earth's anisotropic structure, as well as the practice in
Southern California that enables us to infer the state of the
stress and strain in the lithosphere and the dynamics of the
asthenospheric mantle flow for a better understanding of the
strength and deformation in the upper mantle beneath the San
Andreas Fault system.
This book presents investigations on the Earth's seismic structure
using both active-source and natural earthquake records. It
discusses the ground-truth data obtained from the TAiwan Integrated
GEodynamics Research (TAIGER) active-source experiments that
provides excellent and unique insights into the shallow crustal
structures beneath Taiwan. It also explores the full-wave
sensitivity kernels, which account for the effects of all possible
wave interferences involved in shear-wave splitting and therefore
loosen the restrictions on source-receiver geometry amenable to
shear-wave splitting analysis. Moreover, it describes the 3D
Frechet kernels, which enable us to resolve the vertical and
lateral variations in seismic anisotropy and obtain 3D images of
the Earth's anisotropic structure, as well as the practice in
Southern California that enables us to infer the state of the
stress and strain in the lithosphere and the dynamics of the
asthenospheric mantle flow for a better understanding of the
strength and deformation in the upper mantle beneath the San
Andreas Fault system.
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