1887

Abstract

The Late Cretaceous-Danian Chalk Group is buried at depths varying from 0 to more than 3 km in the<br>North Sea Basin. Nature has thus conducted a dramatic experiment that allows us to study the effect of this<br>large depth variation on the seismic velocity and hence on the compaction of the chalk.

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/content/papers/10.3997/2214-4609.201407552
1994-09-09
2020-09-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407552
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