Adjoint-state traveltime tomography for azimuthally anisotropic media and insight into the crustal structure of central California near Parkfield
Seismic anisotropy provides crucial information on the stress state and geodynamic processes inside the Earth. We develop a novel adjoint-state traveltime tomography method using P-wave traveltime data to simultaneously determine velocity heterogeneity and azimuthal anisotropy of the subsurface. Fir...
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格式: | Article |
語言: | English |
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2021
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在線閱讀: | https://hdl.handle.net/10356/153558 |
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