Marine multicomponent seismology has seized the geophysical industry’s fancy since its semicommercial emergence in the North Sea in the autumn of 1996. The essence of this technology is recording S-waves, in addition to conventional P-waves, on the seafloor with sensor packages containing hydrophones and three-component geophones. New processing algorithms have had to be developed to properly process these data.
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Jack Caldwell (1999) studied this question.
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