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Isotropic and anisotropic seismic to...
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Lin, Yu-Pin.
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Isotropic and anisotropic seismic tomography using active source and earthquake records
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Isotropic and anisotropic seismic tomography using active source and earthquake records/ by Yu-Pin Lin.
作者:
Lin, Yu-Pin.
出版者:
Singapore :Springer Singapore : : 2018.,
面頁冊數:
xxvii, 91 p. :ill., digital ;24 cm.
內容註:
Introduction -- Assessment of Tomography Models of Taiwan Using First-arrival Times from the TAIGER Active-source Experiment -- Crustal Velocity Variations in Taiwan Revealed by Active-source Seismic Observations -- Full-wave Effects on Shear-wave Splitting -- Full-wave Multiscale Anisotropy Tomography in Southern California -- Concluding Remarks.
Contained By:
Springer eBooks
標題:
Seismic tomography. -
電子資源:
http://dx.doi.org/10.1007/978-981-10-5068-8
ISBN:
9789811050688
Isotropic and anisotropic seismic tomography using active source and earthquake records
Lin, Yu-Pin.
Isotropic and anisotropic seismic tomography using active source and earthquake records
[electronic resource] /by Yu-Pin Lin. - Singapore :Springer Singapore :2018. - xxvii, 91 p. :ill., digital ;24 cm. - Springer theses,2190-5053. - Springer theses..
Introduction -- Assessment of Tomography Models of Taiwan Using First-arrival Times from the TAIGER Active-source Experiment -- Crustal Velocity Variations in Taiwan Revealed by Active-source Seismic Observations -- Full-wave Effects on Shear-wave Splitting -- Full-wave Multiscale Anisotropy Tomography in Southern California -- Concluding Remarks.
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.
ISBN: 9789811050688
Standard No.: 10.1007/978-981-10-5068-8doiSubjects--Topical Terms:
668242
Seismic tomography.
LC Class. No.: QE538.5
Dewey Class. No.: 551.22
Isotropic and anisotropic seismic tomography using active source and earthquake records
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Introduction -- Assessment of Tomography Models of Taiwan Using First-arrival Times from the TAIGER Active-source Experiment -- Crustal Velocity Variations in Taiwan Revealed by Active-source Seismic Observations -- Full-wave Effects on Shear-wave Splitting -- Full-wave Multiscale Anisotropy Tomography in Southern California -- Concluding Remarks.
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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.
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