1887

Abstract

Stratigraphic studies of Late Cretaceous sequences in northwest Europe frequently fail to<br>identify subtIe changes in both lithofacies and biofacies due to the apparent monotonous nature<br>of chalk sediments. This results in the non-recognition of many major factors affecting the<br>stratigraphic succession, well geohistories and the mis-interpretation of regional sequentiaI<br>history.

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/content/papers/10.3997/2214-4609.201407529
1994-09-09
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407529
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