Evidence for fluid migration following pockmark formation: Examples from the Nile Deep Sea Fan
A large number of pockmarks have been identified in the Rosetta Region of the Western Nile Deep Sea Fan. Co-located high resolution 2D and Chirp datasets have been used to identify seabed and buried pockmarks which are interpreted to span the Holocene to Pleistocene period. The pockmarks range in si...
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Veröffentlicht in: | Marine geology 2012-03, Vol.303-306, p.1-13 |
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