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METHOD OF SEISMIC EXPLORATION OF A MEDIUM, ESPECIALLY OF GEOPHYSICAL PROSPECTION BY SEISMIC WAVES

机译:介质的地震勘探方法,尤其是通过地震波进行地球物理勘探的方法

摘要

P THIS PROCESS CONSISTS OF EMITTING A FIRST SEQUENCE OF N MECHANICAL PULSES SEPARATED BY TIMES EQUAL T FOLLOWED BY A LISTENING TIME AT LEAST EQUAL TO THE TURN-BACK TIME OF A PULSE FROM THE GROUND TO THE DEEPEST LAYER, AT CORRELATE THE SIGNALS RECEIVED, TO ISSUED A SECOND SEQUENCE OF N SEPARATED PULSES BY TIMES EQUAL TO D DIFFERENT FROM T, TO PROCEED AS PREVIOUSLY, TO ISSUING A SUFFICIENT NUMBER OF SEQUENCES NI, TI, TO BE THE RESULTS OF THE DIFFERENT, CORRELATIONS TI, AS THE SUM OF THE SELF-CORRECTING FUNCTIONS IS IN THE FORM OF A CENTRAL PIC OF AMPLITUDE NN N ... NOR FRAME OF SECONDARY PICS WITH A RATIO SUPERIOR TO THE REPORT OF THE AMPLITUDES OF SIGNALS RECEIVED IN INTERVALS OF TIME CORRESPONDING TO INTERVALS SEPARATING THE MAIN PIC OF EACH OF THE SECONDARY PICS. /P
机译:

此过程包括发出N个机械脉冲的第一个序列,该序列的时间等于T的时间,其次是从听见时间到从地面到深度层的脉冲返回时间(至少与信号相关) ,由N个分开的脉冲的第二个序列,从T到D的时间相等,然后按顺序进行,以产生足够数量的序列NI,TI,作为不同的相关性TI的结果。自我校正功能的形式为幅度为NN N ...的中央图片,而次级图片的帧数与比例对应于主间隔的时间间隔中接收到的信号幅度的报告比率成正比每个中学图片。

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