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JanThorbecke
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debugging info
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extrap/doc/OpenExtrap.pdf

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extrap/doc/OpenExtrap.tex

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% Make a version of the title for latex and html
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\newdimen{\mybaselineskip}
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\mybaselineskip=24pt
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\title{OpenExtrap 1.0}
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\title{OpenExtrap 1.1}
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\author{Jan W. Thorbecke}
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extrap/doc/migr.tex

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\subsection{General parameter description}
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The shots to be migrated ({\tt file\_shot}) and the gridded subsurface files ({\tt file\_vel} and {\tt file\_vels}) should have the same lateral extend being defined by the {\tt gx} headers. The position of the receivers of the data in the subsurface grid is done by means of the {\tt gx} header value of the velocity model corresponding to the {\tt gx} header value in the data to be extrapolated. The distance between the traces in the velocity model should be smaller or equal to the distance between the receivers/shots. The program assigns the {\tt gx} value of the receivers to the nearest grid point in the velocity model. The number of depth steps is controlled with the parameter {\tt ndepth=}. To avoid reflections at the edges of the model the parameter {\tt ntap} can be set. {\tt ntap} indicates the number of points at the edges for which a spatial taper is designed according to: $\exp{(-(0.4*(ntap-ix)/ntap)^2)}$. Choosing {\tt ntap} equal to half of the operator length is an optimimum value.
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The shots to be migrated ({\tt file\_shot}) and the gridded subsurface files ({\tt file\_vel} and {\tt file\_vels}) should have the same lateral extend being defined by the {\tt gx} headers. The position of the receivers of the data in the subsurface grid is done by means of the {\tt gx} header value of the velocity model corresponding to the {\tt gx} header value in the data to be extrapolated. The distance between the traces in the velocity model should be smaller or equal to the distance between the receivers/shots. The program assigns the {\tt gx} value of the receivers to the nearest grid point in the velocity model. The number of depth steps is controlled with the parameter {\tt ndepth=}. To avoid reflections at the edges of the model the parameter {\tt ntap} can be set. {\tt ntap} indicates the number of points at the edges for which a spatial taper is designed according to: $\exp{(-(0.4*(ntap-ix)/ntap)^2)}$. Choosing {\tt ntap} equal to half of the operator length is an optimum value.
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The {\tt sx} or {\tt fldr} headers in {\tt file\_shot} determine a single shor record. As long as {\tt sx} or {\tt fldr} header value remain constant the program considers these traces belonging to a single shot. If one of these values changes this trace is then considered to belong to the next shot. Be careful for example with common-offset data. In this kind of data set the {\tt sx} or {\tt fldr} header value usually change with each trace, hence each trace is considered to be one shot by the program. To overcome this problem set {\bf both} {\tt sx} or {\tt fldr} header values to a constant value
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Topography is taken into account by using a velocity model which has zero velocities above the defined topography. In that case the position of the source and receivers is lowered into the velocity model until a non-zero velocity is found. From that depth the extrapolation of that point is started.
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