SUTIHALEDMO - TI Hale Dip MoveOut (based on Hale's PhD thesis)	  sutihaledmo <infile >outfile [optional parameters]			 Required Parameters:							 nxmax		  maximum number of midpoints in common offset gather Optional Parameters:							 option=1		1 = traditional Hale DMO (from PhD thesis)				2 = Bleistein's true amplitude DMO					3 = Bleistein's cos*cos weighted DMO					4 = Zhang's DMO								5 = Tsvankin's anisotropic DMO						6 = Tsvankin's VTI DMO weak anisotropy approximation dx=50.		 midpoint sampling interval between traces				in a common offset gather.  (usually shot				interval in meters)				 v=1500.0		velocity (in meters/sec)						(must enter a positive value for option=3)				(for excluding evanescent energy)		 h=200.0		source-receiver half-offset (in meters)		 ntpad=0		number of time samples to pad			 nxpad=h/dx		number of midpoints to pad			 file=vnmo		name of file with vnmo as a function of p				used for option=5--otherwise not used					(Generate this file by running program					sutivel with appropriate list of Thomsen's				parameters.)					 e=0.			Thompsen's epsilon				 d=0.			Thompsen's delta				Note:									 This module assumes a single common offset gather after NMO is	 to be input, DMO corrected, and output.  It is useful for computing	 theoretical DMO impulse responses.  The Hale algorithm is		 computationally intensive and not commonly used for bulk processing	 of all of the offsets on a 2-D line as there are cheaper alternative	 algorithms.  The Hale algorithm is commonly used in theoretical studies. Bulk processing for multiple common offset gathers is typically done	 using other modules.							 Test run:   suspike | sutihaledmo nxmax=32 option=1 v=1500 | suxwigb &  Author:  (Visitor to CSM from Mobil) John E. Anderson Spring 1994 References: Anderson, J.E., and Tsvankin, I., 1994, Dip-moveout by	Fourier transform in anisotropic media, CWP-146