Patent GB-993431-A (GB)
Title: Improvements in methods of exploiting seismic recordings
IPC: G06E3/00
Filed: 1962-01-25
Abstract: 993,431. Seismic prospecting. COMPAGNIE GENERALE DE GEOPHYSIQUE. Jan. 25, 1962 [Jan. 27, 1961], No. 2935/62. Heading H4D. The Specification relates to a method of processing records derived in geophysical prospecting and describes automatic means whereby " static " and " dynamic " corrections may be effected and a single correlated record produced. Essentially, the method consists of evaluating #=#<SP>t</SP> Y dt (where Y=#2ab= (a+b+c+d)<SP>2</SP>-(a<SP>2</SP>+b<SP>2</SP>+c<SP>2</SP>+d<SP>2</SP>)<SP>t-T2</SP>, a, b, c and d being the ordinates of four consecutive or regularly spaced traces evaluated at instant t-3# 1 /2, t-# 1 /2, t+# 1 /2 and t+3# 1 /2 respectively and 0, a selected value for the time gradient between adjacent traces. The integration is effected over an interval T 2 (=20 to 50 milliseconds) for different values of t and repeated for different values of # 1 . Alternatively, the integral may be of the form #<SP>1</SP> =# 0 <SP>t</SP> e u-t/T Y(u)du where Y(u) is the ordinate   of a first trace at the instant u. In addition to the above integration the sum #=a+b+c+d is evaluated as a function of time and a family of curves is produced having ordinates # Î # plotted against time, each corresponding to a particular combination of the four initial seismic traces and a particular value of # 1 . Fig. 2 shows an automatic arrangement for producing a correlated record employing the function #<SP>1</SP> as the co-efficient of correlation. In this arrangement pre-recorded electrical signals (voltages) corresponding to the ordinates of the traces a, b, c and d are derived from a rotating magnetic tape store 23 and supplied to respective delay lines T to 4 which effect delays - 3# 1 /2, - # 1 /2, + # 1 /2, + 3# 1 /2 the negative delays (i.e. advances) being obtained by corresponding delays applied to the other voltages and the actual value of # 1  being adjustable by means of a single control member 9. The signals from the delay lines are combined in a member 10 to form the quantity Y which is integrated to produce the function #<SP>1</SP> in a low-pass filter 12 the cut-off frequency of which is adjustable between 16 c.p.s. (T 2 =60 milliseconds) and 32 c.p.s. (T 2 =30 milliseconds). The outputs of the delay lines are also fed to an adder 13 together with the output of filter 12 and the signal from adder 13 is differentiated in 14 and the differentiated signal supplied to a discriminator 15 which produces an output pulse each time the input from 14 passes through zero. This pulse is employed to trigger a rectangular wave generator 16 the width (duration) of the output wave of which is a function of the instantaneous value of the signal output of filter 12. The output of generator 16 is then utilized as a brightening pulse for cathode-ray tube 18 the beam of which is deflected in both vertical and horizontal direction by saw-tooth waves from generator 19. The amplitude of the vertical deflection however is controlled by the member 9 which also controls the delay # 1  of the delay lines 1 to 4, so that, with a fixed amplitude of horizontal deflection (pre-set in accordance with the spacing between consecutive seismic traces) the trace produced on the screen of tube 18 is a straight line the inclination of which is a function of # 1  and the thickness of which is proportional to the function #<SP>1</SP>. This trace is recorded on photographic paper carried by a drum 22 rotating with drum 23, as many recordings (successively superimposed) being made for each group of four seismic traces as there are values of # 1  investigated. Specification 993,432 is referred to.