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📄 suattributes.su.main

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 SUATTRIBUTES - instantaneous trace ATTRIBUTES 			 suattributes <stdin >stdout mode=amp					 Required parameters:							 	none								 Optional parameter:							 	mode=amp	output flag 					 	       		=amp envelope traces				 	       		=phase phase traces				 	       		=freq frequency traces							=freqw Frequency Weighted Envelope					=thin  Thin-Bed (inst. freq - average freq)				=bandwith Instantaneous bandwidth					=normamp Normalized Phase (Cosine Phase)	 	       		=fdenv 1st envelope traces derivative		 	       		=sdenv 2nd envelope traces derivative		 	       		=q Ins. Q Factor					unwrap=		default unwrap=0 for mode=phase			 			default unwrap=1 for mode=freq			 			dphase_min=PI/unwrap					wint=		windowing for freqw							windowing for thin							default=1 					 			o--------o--------o				 			data-1	data	data+1				 Notes:								 This program performs complex trace attribute analysis. The first three attributes, amp,phase,freq are the classical Taner, Kohler, and	 Sheriff, 1979.							 The unwrap parameter is active only for mode=freq and mode=phase. The	 quantity dphase_min is the minimum change in the phase angle taken to be the result of phase wrapping, rather than natural phase variation in the data. Setting unwrap=0 turns off phase-unwrapping altogether. Choosing unwrap > 1 makes the unwrapping function more sensitive to phase changes. Setting unwrap > 1 may be necessary to resolve higher frequencies in	 data (or sample data more finely). The phase unwrapping is crude. The  differentiation needed to compute the instantaneous frequency		 freq(t)= d(phase)/dt is a simple centered difference.			 Examples:								 suvibro f1=10 f2=50 t1=0 t2=0 tv=1 | suattributes2 mode=amp | ...	 suvibro f1=10 f2=50 t1=0 t2=0 tv=1 | suattributes2 mode=phase | ...	 suvibro f1=10 f2=50 t1=0 t2=0 tv=1 | suattributes2 mode=freq | ...	 suplane | suattributes mode=... | supswigb |...       		 Credits:	CWP: Jack Cohen      CWP: John Stockwell (added freq and unwrap features)	UGM (Geophysics Students): Agung Wiyono           email:aakanjas@gmail.com (others)					 Algorithm:	c(t) = hilbert_tranform_kernel(t) convolved with data(t)    amp(t) = sqrt( c.re^2(t) + c.im^2(t))  phase(t) = arctan( c.im(t)/c.re(t))  freq(t) = d(phase)/dt Reference: Taner, M. T., Koehler, A. F., and  Sheriff R. E. "Complex seismic trace analysis", Geophysics,  vol.44, p. 1041-1063, 1979 Trace header fields accessed: ns, trid Trace header fields modified: d1, trid

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