Why a big 2-D array to record microseisms? , by Jon Claerbout, Steve Cole, Dave Nichols, and Lin Zhang

We plan to set out a two-dimensional seismic array, with our 200 group recorders. The initial goal is to measure an emergent angle spectrum of the microseismic noise. Our array will be designed to attenuate surface-travelling noise as musch as possible. The dominant steeply emerging energy is expected to be generated by the ocean surf20km distant. Such energy should enable imaging by the theorem that the (slant stacked) autocorrelation of the microseism is the reflection seismogram. Ultimately we hope to reproduce a portion of a conventional reflection image, and extend it in frequency or depth.


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