Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method

Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 1999.

Bibliographic Details
Main Author: Sierra T., Jesús V. (Jésus Vicente), 1965-
Other Authors: M. Nafi Toksöz.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2010
Subjects:
Online Access:http://hdl.handle.net/1721.1/58164
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author Sierra T., Jesús V. (Jésus Vicente), 1965-
author2 M. Nafi Toksöz.
author_facet M. Nafi Toksöz.
Sierra T., Jesús V. (Jésus Vicente), 1965-
author_sort Sierra T., Jesús V. (Jésus Vicente), 1965-
collection MIT
description Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 1999.
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institution Massachusetts Institute of Technology
language eng
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spelling mit-1721.1/581642020-05-08T16:34:16Z Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method Sierra T., Jesús V. (Jésus Vicente), 1965- M. Nafi Toksöz. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Earth, Atmospheric, and Planetary Sciences Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 1999. Includes bibliographical references (leaves 116-119). We present an original method for estimating local shear wave birefringence properties for 3D surface P to S converted waves. To accomplish this we approach the problem using reverse VSP (RVSP). The method works in the pre-stack domain and uses the P waves converted to S as shear wave sources. We solve the transmission problem using the propagator matrix method. The importance of this method is that it does not require information about layering above the zone of interest and is accurate for estimating the anisotropy parameters. The method involves solving a non-linear problem in the frequency domain where Simulated Annealing is used as the global minimization technique. The procedure allows estimation of the propagator matrix related to the target zone, assuming plane wave propagation allows its diagonalization by pure rotations. This matrix diagonalization ends up with an estimation of the natural eigen directions of the medium when the range of offset angles does not exceed 35*. The proposed method is validated with synthetic RVSP data for two models with different densities of vertical fractures. Results show good accuracy in the estimation of the angle of the fractures for the whole range of offsets. The study also extends to show the dependence on the frequency and on the offset. by Jesús V. Sierra T. S.M. 2010-09-02T14:48:26Z 2010-09-02T14:48:26Z 1998 1999 Thesis http://hdl.handle.net/1721.1/58164 42731648 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 119 leaves application/pdf Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences
Sierra T., Jesús V. (Jésus Vicente), 1965-
Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title_full Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title_fullStr Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title_full_unstemmed Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title_short Interpretation of shear wave birefringence in P to S converted waves data using the propagator matrix method
title_sort interpretation of shear wave birefringence in p to s converted waves data using the propagator matrix method
topic Earth, Atmospheric, and Planetary Sciences
url http://hdl.handle.net/1721.1/58164
work_keys_str_mv AT sierratjesusvjesusvicente1965 interpretationofshearwavebirefringenceinptosconvertedwavesdatausingthepropagatormatrixmethod