tomo
所属分类:其他
开发工具:matlab
文件大小:20KB
下载次数:10
上传日期:2018-12-02 18:43:48
上 传 者:
Zigzag-j
说明: tomo3d主要用于联合折射波和反射波进行近地表速度建模,可以利用该方法为全波形提供较好的初始速度模型。
(Tomo3d is mainly used to model near-surface velocity by combining refraction wave and reflection wave. This method can be used to provide a better initial velocity model for full waveform.)
文件列表:
tomo (0, 2018-10-01)
tomo\.__afs169E (0, 2006-11-28)
tomo\.travel_times.m.swp (12288, 2006-11-29)
tomo\bgls_interface.dat (20989, 2018-11-18)
tomo\bgls_ttimes.dat (30048, 2018-11-18)
tomo\make_data.m (4744, 2006-11-29)
tomo\travel_times.m (1563, 2006-11-29)
tomo\ttime.m (3505, 2006-11-29)
tomo\新建文本文档.txt (98, 2018-06-16)
The Seismic Reflection Tomography problem
^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^
This file contains the Matlab programs that have been used to realize
the unconstrained optimization example described in section 7 (A Case
Study: Seismic Reflection Tomography) of the book
Numerical Optimization - Theoretical and Practical Aspects
(Second Edition)
by J. Frédéric Bonnans, J. Charles Gilbert, Claude Lemaréchal, and
Claudia A. Sagastizábal
Springer, series Universitext, 2006, XIV, 494 p., 52 illus., Softcover
ISBN-10: 3-540-35445-X
ISBN-13: 978-3-540-35445-1
See http://www-rocq.inria.fr/~gilbert/bgls for more information on this
so-called BGLS book.
The problem can be used (and has been used) as a computational exercise
in unconstrained numerical optimization for students learning this
discipline. In the following, we describe the problem and explain how
to use the Matlab files of the problem directory. Firther information
is contained in the book.
REQUIREMENTS: The programs use the "Optimization" and "Spline"
toolboxes of Matlab.
1) Introduction
^^^^^^^^^^^^^^^
Seismic reflection tomography is a method for determining a subsurface
velocity model from the traveltimes of seismic waves reflecting on
geological interfaces. In this simplified example, we are just
interested in recovering the position of a reflection interface,
discarding the recovering of the wave velocity, which is supposed to be
the constant one. From an optimization viewpoint, the problem consists
in minimizing a nonlinear least-squares function measuring the mismatch
between observed traveltimes and those calculated by ray tracing in
this model.
2) Building the data
^^^^^^^^^^^^^^^^^^^^
In Matlab, by typing
make_data
the data related to the step-pyramid interface are built and stored in
the files
bgls_interface.dat: description of the
bgls_ttimes.dat: travel times of the rays reflecting on the
step-pyramid interface from sources to receivers.
The program uses the following Matlab functions:
travel_times: computes all the travel times
ttime: computes a single travel time for a given source and receiver.
During the computation of the travel times, the ray tracing show the
rays on the plot. This operation can take a while ...
References
^^^^^^^^^^
F. Delbos, J.Ch. Gilbert, R. Glowinski, and D. Sinoquet. Constrained
optimization in seismic reflection tomography: a Gauss-Newton augmented
Lagrangian approach. Geophysical Journal International, 1***:670-684,
2006.
F. Delprat-Jannaud and P. Lailly. What information on the Earth model
do reflection travel times hold? Journal of Geophysical Research,
97:1***27-1***44, 1992.
F. Delprat-Jannaud and P. Lailly. Ill-posed and well-posed formulations
of the reflection travel time tomography problem. Journal of
Geophysical Research, ***:6589-6605, 1993.
R. Glowinski and Q.-H. Tran. Constrained optimization in reflexion
tomography: the augmented Lagrangian method. East-West J. Numer. Math.,
1(3):213-234, 1993.
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