1887

Abstract

Classically, the North-Sea Chalk is assumed to have deposited under quiet, homogeneous pelagic conditions with local redeposition in slumps and slides. However, in recent times the observation of highly discontinuous reflection patterns on 2D and 3D seism

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/content/papers/10.3997/2214-4609.201400561
2009-06-08
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400561
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