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 SUDMOFKCW - converted-wave DMO via F-K domain (log-stretch) method for 		common-offset gathers					 sudmofkcw <stdin >stdout cdpmin= cdpmax= dxcdp= noffmix= [...]	 Required Parameters:							 cdpmin		  minimum cdp (integer number) for which to apply DMO cdpmax		  maximum cdp (integer number) for which to apply DMO dxcdp		   distance between adjacent cdp bins (m)		 noffmix		 number of offsets to mix (see notes)		 Optional Parameters:							 tdmo=0.0		times corresponding to rms velocities in vdmo (s) vdmo=1500.0		rms velocities corresponding to times in tdmo (m/s) gamma=0.5		 velocity ratio, upgoing/downgoing		 ntable=1000		 number of tabulated z/h and b/h (see notes)	 sdmo=1.0		DMO stretch factor; try 0.6 for typical v(z)	 flip=0		 =1 for negative shifts and exchanging s1 and s2 			 (see notes below)				 fmax=0.5/dt		maximum frequency in input traces (Hz)		 verbose=0		=1 for diagnostic print				 Notes:								 Input traces should be sorted into common-offset gathers.  One common- offset gather ends and another begins when the offset field of the trace headers changes.							 The cdp field of the input trace headers must be the cdp bin NUMBER, NOT the cdp location expressed in units of meters or feet.		 The number of offsets to mix (noffmix) should typically equal the ratio of the shotpoint spacing to the cdp spacing.  This choice ensures that every cdp will be represented in each offset mix.  Traces in each mix will	 contribute through DMO to other traces in adjacent cdps within that mix. The tdmo and vdmo arrays specify a velocity function of time that is	 used to implement a first-order correction for depth-variable velocity. The times in tdmo must be monotonically increasing. The velocity function is assumed to have been gotten by traditional NMO. 			 For each offset, the minimum time at which a non-zero sample exists is used to determine a mute time.  Output samples for times earlier than this",  mute time will be zeroed.  Computation time may be significantly reduced if the input traces are zeroed (muted) for early times at large offsets. z/h is horizontal-reflector depth normalized to half source-reciver offset h.  Normalized shift of conversion point is b/h.  The code now does not support signed offsets, therefore it is recommended that only end-on data, not split-spread, be used as input (of course after being sorted into	 common-offset gathers).  z/h vs b/h depends on gamma (see Alfaraj's Ph.D. thesis, 1993).							 Flip factor = 1 implies positive shift of traces (in the increasing CDP bin number direction).  When processing split-spread data, for example, if one side of the spread is processed with flip=0, then the other side of the spread should be processed with flip=1.  The flip factor also	 determines the actions of the factors s1 and s2, i.e., stretching or	 squeezing.								 Trace header fields accessed:  nt, dt, delrt, offset, cdp.		 Credits:	CWP: Mohamed Alfaraj		Dave Hale Technical Reference:	Transformation to zero offset for mode-converted waves	Mohammed Alfaraj, Ph.D. thesis, 1993, Colorado School of Mines	Dip-Moveout Processing - SEG Course Notes	Dave Hale, 1988

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