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 SUSTATICRRS - Elevation STATIC corrections, apply corrections from		      headers or from a source and receiver statics file,		      includes application of Residual Refraction Statics	     sustaticrrs <stdin >stdout  [optional parameters]	 		 Required parameters:								none								 Optional Parameters:								v0=v1 or user-defined	or from header, weathering velocity		v1=user-defined		or from header, subweathering velocity		hdrs=0			=1 to read statics from headers		 				=2 to read statics from files			sign=1			=-1 to subtract statics from traces(up shift) Options when hdrs=2:								sou_file=		input file for source statics (ms) 		rec_file=		input file for receiver statics (ms) 		ns=240 			number of sources 				nr=335 			number of receivers 				no=96 			number of offsets			 Options when hdrs=3:                                                         blvl_file=              base of the near-surface model file (sampled                                  at CMP locations)                           refr_file=              horizontal reference datum file (sampled at                                  CMP locations)                              nsamp=                  number of midpoints on line                    fx=                     first x location in velocity model             dx=                     midpoint interval                              V_r=                    replacement velocity                           mx=                     number of velocity model samples in                                       lateral direction                           mz=                     number of velocity model samples in                                       vertical direction                          dzv=                    velocity model depth interval                  vfile=                  near-surface velocity model              Options when hdrs=4:                                                         nsamp=                  number of midpoints on line                    fx=                     first x location in velocity model      ",        dx=                     midpoint interval                       ",  Options when hdrs=5:                                                         none                                                             Notes:								 For hdrs=1, statics calculation is not performed, statics correction   is applied to the data by reading statics (in ms) from the header.	 For hdrs=0, field statics are calculated, and				 	input field sut is assumed measured in ms.			 	output field sstat = 10^scalel*(sdel - selev + sdepth)/swevel	 	output field gstat = sstat - sut/1000.				 	output field tstat = sstat + gstat + 10^scalel*(selev - gelev)/wevel For hdrs=2, statics are surface consistently obtained from the 	 statics files. The geometry should be regular.			 The source- and receiver-statics files should be unformated C binary 	 floats and contain the statics (in ms) as a function of surface location. For hdrs=3, residual refraction statics and average refraction statics are computed.  For hdrs=4, residual refraction statics are applied,    and for hdrs=5, average refraction statics are applied (Cox, 1999).    These three options are coupled in many data processing sequences:     before stack residual and average refraction statics are computed but  only residual refractions statics are applied, and after stack average refraction statics are applied.  Refraction statics are often split    like this to avoid biasing stacking velocities.  The files blvl_file   and refr_file are the base of the velocity model defined in vfile and  the final reference datum, as described by Cox (1999), respectively.   Residual refraction statics are stored in the header field gstat, and  the average statics are stored in the header field tstat.  V_r is the  replacement velocity as described by Cox (1999).  The velocity file,   vfile, is designed to work with a horizontal upper surface defined in  refr_file.  If the survey has irregular topography, the horizontal     upper surface should be above the highest topographic point on the     line, and the velocity between this horizontal surface and topography  should be some very large value, such as 999999999, so that the        traveltimes through that region are inconsequential.                   Credits:	CWP: Jamie Burns	CWP: Modified by Mohammed Alfaraj, 11/10/1992, for reading	     statics from headers and including sign (+-) option      CWP: Modified by Timo Tjan, 29 June 1995, to include input of           source and receiver statics from files.       CWP: Modified by Chris Robinson, 11/2000, to include the splitting           of refraction statics into residuals and averages Trace header fields accessed:  ns, dt, delrt, gelev, selev,	sdepth, gdel, sdel, swevel, sut, scalel Trace header fields modified:  sstat, gstat, tstat References: Cox, M., 1999, Static corrections for seismic reflection surveys:    Soc. Expl. Geophys.

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