Page 301 - Acquisition and Processing of Marine Seismic Data
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292                                   5. PREPROCESSING


































           FIG. 5.55  (A) Two filtered shots with dominant swell noise between channels 130 and 160 (indicated by blue arrows).
           (B) After killing the traces with high amplitude swell noise.



           streamer approaches to the sea surface, possibly  new line during the acquisition (Section 2.5.1.9).
           because of a nonfunctional or miscalibrated  However, if the line is too close to the land, or
           bird, and the hydrophones on this part of the  if there is an obstruction in the maneuvering area
           streamer receive a large amount of swell noise.  such as marine traffic or production platforms,
           Fig. 5.55A shows two filtered shot gathers con-  then it may not be possible to fulfill the entire
           taminated by swell noise between channel num-  run-in distance, and in this case, recording can
           bers 130 and 160. Their amplitudes are so high  be initiated before the streamer finishes its turn
           that it is sometimes impossible to recover reflec-  completely. This results in recording with far
           tion amplitudes behind the swell noise. In such  channels that are still turning behind the vessel.
           cases, the most appropriate way to remove the  During their turn, these channels will be closer
           swell noise is to kill the traces dominated by  to the gun array than they normally should be,
           swell noise amplitudes, as in Fig. 5.55B.    which means that these channels will record
              When the vessel maneuvers from one line to  the reflections earlier than their expected arrival
           another during the line changes, streamers bend  times. That is, a curved zone of the reflection
           behind the vessel and, depending on the length of  amplitudes occurs at far offsets of the shot
           the streamer(s), it takes a considerable time for  gathers. Fig. 5.56A shows a number of shots from
           streamers to become straight again, even if the  the beginning of a 2D seismic line with such
           vessel itself is already on the survey line. That  curved zones indicated by blue arrows. This zone
           is why we use run-in distance when entering a  appears at the very first shots of the survey lines,
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