Abstract
Many of the processing systems currently available treat each part of a marine seismic spread as a collection of discrete units — individual compasses on individual streamers, individual acoustic transponders on individual gun strings and so on. Even acoustic networks are treated individually — a network at the front of the spread, one at the tail of the streamers and perhaps another in the centre. This ‘individualism’ even goes so far as to treat each time event on its own.
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© 1997 Springer Science+Business Media Dordrecht
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Loweth, R.P. (1997). Kalman filters. In: Manual of Offshore Surveying for Geoscientists and Engineers. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5826-8_5
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DOI: https://doi.org/10.1007/978-94-011-5826-8_5
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-6461-3
Online ISBN: 978-94-011-5826-8
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