Computation of MULTI-VALUED TRAVELTIMES in the
Marmousi model
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We propose a smooth version of the Marmousi model.
The model is sampled to a 24 by 24 m grid. It
contains 384 samples in the x-direction and 122 samples in the z-direction.
Hence, it is precisely 9192 m long and 2904 m deep.
The smooth model is obtained from a 'hard' model by convolving with a spatial
Hanning (cos^2) filter of radius 150 m.
You can download the compressed files containind this models
(do not forget to select the option save file
or load to local disk).
They were written under the following format :
DO IX=1,384
DO IZ=1,122
WRITE(FILE,1) V(IX,IZ)
ENDDO
ENDDO
1 FORMAT(F8.0)
The source point for the proposed experiment
is located at X=6000m and Z=2800m. A
BLACK CROSS
indicates its location on the smooth Marmousi
model.
We propose that the receivers be sampled
at the surface every 24m. That is at
every grid point location.
Dowload the SMOOTH model and solve the problem for the multivalued
travel time field (at least at the surface) with your favourite
method.
The displayed results will consist of the plot of all traveltimes
recorded at the surface receivers. There are 384 receivers equally
spaced every 24 meters from 0 to 9192 meters at the surface (every grid
point).
The result should be in the form of an ascii file containing
only one arrival on each line. Each arrival will be described
with two numbers :
The receiver number (from 1 to 384) /a space/ the recorded arrival time (in seconds)
For example, if you only recorded three arrivals at the surface,
at time 1.3 s. at the receiver situated at 288 m., 1.278 s.
at 3672 m. and 0.45 s. at 3672 m. again (a multi-valued arrival position),
then your file will be of the form :
12 1.3
153 1.278
153 0.45
Then send your ascii file to :
Jean-David.Benamou@inria.fr
A ray tracing simulation.
A Big Ray Tracing simulation.
A wavefront construction simulation from NORSAR
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