1887

Abstract

The Moesian Platform was the depocenter for 700-1,200 m thick Malm- Neocomian carbonate deposits. The stratigraphic interpretation of the seismic sections together with drilling, laboratory, regional and general geologic data led to the identification of numerous bioherms and biostromes. They are the subject of the paper.

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/content/papers/10.3997/2214-4609.201409619
1995-05-29
2020-11-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409619
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