Seismic clock timing correction using ocean acoustic waves

摘要

A method for identifying clock timing discrepancies in at least one clock of interest that is associated with a marine seismic receiver, comprises collecting from at least one marine receiver other than the receiver of interest a first data set corresponding to a selected time period, said first data set being selected to include ocean wave signals; collecting from the receiver of interest a second data set corresponding to the selected time period, said second data set being selected to include ocean wave signals; applying a mathematical prediction technique to the ocean wave signals in the first data set so as to generate a predicted response for a receiver co-located with the receiver of interest; comparing the predicted response to the second data set so as to generate a correlation data set; and using the correlation data set to determine a corrected parameter for the receiver of interest.

主权项

1. A method for identifying clock timing discrepancies in at least one clock of interest that is associated with a seismic receiver, comprising the steps of:
a) collecting from at least one receiver other than the receiver of interest a first data set corresponding to a selected time period, said first data set being selected to include ocean wave signals recorded at a frequency of ocean waves caused by omnidirectional propagating acoustic noise, wherein there is a receiver spacing between the at least one receiver other than the receiver of interest and the receiver of interest; b) collecting from the receiver of interest a second data set corresponding to the selected time period, said second data set being selected to include ocean wave signals recorded at the frequency of ocean waves caused by the same omnidirectional propagating acoustic noise; c) with a computer generating a predicted ocean wave signal response for a receiver at a new location from the ocean wave signals recorded at a frequency of ocean waves in the first data set, whereby the new location is selected to be co-located with the receiver of interest; d) with the computer comparing the predicted ocean wave signal response to ocean wave signals recorded at a frequency of ocean waves in the second data set so as to generate a correlation data set; and e) with the computer using the correlation data set to determine clock timing error of the receiver of interest; and f) with the computer correcting the clock timing of the receiver of interest by accounting for the clock timing error; wherein the receiver spacing is smaller than a wavelength of the omnidirectional propagating acoustic noise that causes the ocean wave signals.