The study of anisotropy by controlled directional source method : Modeling

博士 === 國立中央大學 === 地球物理學系 === 84 === The purpose of this study is to find a new technique to image the p-q slowness surfaces directly from walk-away VSP by a full wave field transformation in layered models. This method, is based mainly on performing the l...

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Main Authors: Chern Chir-Cherng, 陳奇呈
Other Authors: Hsieh Chao-hui
Format: Others
Language:zh-TW
Published: 1996
Online Access:http://ndltd.ncl.edu.tw/handle/88225277109876988881
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spelling ndltd-TW-084NCU001340122016-02-05T04:16:42Z http://ndltd.ncl.edu.tw/handle/88225277109876988881 The study of anisotropy by controlled directional source method : Modeling 利用定向震源法對物理模型之非均向性研究 Chern Chir-Cherng 陳奇呈 博士 國立中央大學 地球物理學系 84 The purpose of this study is to find a new technique to image the p-q slowness surfaces directly from walk-away VSP by a full wave field transformation in layered models. This method, is based mainly on performing the linear Radon transform twice. The first linear Radon transform acts as a τ- p transform, and This method can be applied to any component of 3D/3C WVSP to estimate the corresponding p-q slowness surfaces and to correlate each surface. We conducted both numerical and p velocity polar function for azimuthally anisotropic media. Moreover, through the SH component analysis, the features of S wave splitting can be seen in the p-q slowness surface. Hsieh Chao-hui 謝昭輝 1996 學位論文 ; thesis 136 zh-TW
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description 博士 === 國立中央大學 === 地球物理學系 === 84 === The purpose of this study is to find a new technique to image the p-q slowness surfaces directly from walk-away VSP by a full wave field transformation in layered models. This method, is based mainly on performing the linear Radon transform twice. The first linear Radon transform acts as a τ- p transform, and This method can be applied to any component of 3D/3C WVSP to estimate the corresponding p-q slowness surfaces and to correlate each surface. We conducted both numerical and p velocity polar function for azimuthally anisotropic media. Moreover, through the SH component analysis, the features of S wave splitting can be seen in the p-q slowness surface.
author2 Hsieh Chao-hui
author_facet Hsieh Chao-hui
Chern Chir-Cherng
陳奇呈
author Chern Chir-Cherng
陳奇呈
spellingShingle Chern Chir-Cherng
陳奇呈
The study of anisotropy by controlled directional source method : Modeling
author_sort Chern Chir-Cherng
title The study of anisotropy by controlled directional source method : Modeling
title_short The study of anisotropy by controlled directional source method : Modeling
title_full The study of anisotropy by controlled directional source method : Modeling
title_fullStr The study of anisotropy by controlled directional source method : Modeling
title_full_unstemmed The study of anisotropy by controlled directional source method : Modeling
title_sort study of anisotropy by controlled directional source method : modeling
publishDate 1996
url http://ndltd.ncl.edu.tw/handle/88225277109876988881
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