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Abstract

The Late Cretaceous stratigraphic sequences are widespread and consist of marine shale and limestone ranging in age from the Turonian up to the Maastrichian. In the study area the sequence of the Late Cretaceous is divided into five clearly recognizable formations.

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/content/papers/10.3997/2214-4609.201406021
2000-10-01
2021-10-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406021
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