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The third advantage is the potential for improvement. This email address is already registered with Scribd. It originates in the fluid motions of the outer core. Any local source of seismic noise will reduce the quality of the data, and a larger seismic energy source may be required to overcome this noise. Thus, voids produce a region in the seismic section where layer continuity decreases, and where amplitudes of the reflected waves are attenuated. Attendance is mandatory during this phase of the class. Two common groundwater occurrences.

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The length of the geophone spread should be sufficient to image the bedrock. Planning EPA Series, National Water Well Association, Dublin, OH.