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📄 displvsp

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#! /bin/sh# set -x# Demos shell for sugoupillaud# Albena Mateeva, Jan 29, 2001#---------------------------------------------------------------# An example reflectivity series in rdemo.asc## 2048 samples corresponding to:## a surface reflection coeficient# ( r[0]=-1.0 for this example, i.e., free surface )## and 2047 subsurface interfaces (equally spaced in time).##---------------------------------------------------------------#-------- show example reflectivity ---------------# in this example the two-way time thickness of the subsurface layers is 2msa2b n1=1 < rdemo.asc | suaddhead ns=2048 | sushw key=dt a=2000 > rdemo.susuxgraph < rdemo.su label1="Time (s)" label2="Displacement Reflection \Coeficient" title="REFLECTIVITY SERIES" x2beg=-1 x2end=1 height=600 width=300 &    # COMPUTE AND GRAPH DISPLACEMENT SEISMOGRAMS FOR A SURFACE SOURCE: #------ surface seismogram --------------------------------------------sugoupillaud < rdemo.su | suresamp | \suxgraph label1="Time (s)" label2="Displacement" \	 title="SURFACE SEISMOGRAM" x2beg=-1 x2end=1 height=600 width=300 &#------ receiver burried at 250 ms (250 layers) below the surface ----- sugoupillaud <rdemo.su k=251 | suresamp | \suxgraph label1="Time (s)" label2="Displacement" \	 title="RECEIVER DEPTH 250 ms" x2beg=-1 x2end=1 height=563 width=300  &	 	 #------ receiver burried at 500 ms (500 layers) below the surface ----- sugoupillaud < rdemo.su k=501 | suresamp | \suxgraph label1="Time (s)" label2="Displacement" \	 title="RECEIVER DEPTH 500 ms" x2beg=-1 x2end=1 height=527 width=300  &# REMARK: The length of these seismograms is defined by the default value# of tmax. It coinsides with the arrival of the primary reflection from the# deepest interface. This choice (and any smaller tmax) neutralizes the# consequences of modelling the earth below the deepest interface as a# homogeneous half-space.# SUGGESTED EXERCISE: Change the surface reflection coeficient# (the first entry in the rdemo.asc file) from -1.0 (free surface)# to zero (no surface-related multiples) and see what happens to# the seismograms. exit 0

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