Skip to Main Content
Skip Nav Destination

Callovian to Paleocene strata outcrop in the Varna region of northeast Bulgaria, and have also been recorded from several wells in both the Black Sea and onshore locations to the northeast and the south of Varna in the Kamchia Basin. Sedimentological data collected from the abundant core material recovered from these wells allow detailed facies schemes to be developed and regional paleofacies maps to be constructed.

During the Callovian to Valanginian, eastern Bulgaria and the Bulgarian Black Sea were divided into areas dominated by shallow-marine carbonate sedimentation and deeper water environments. The boundary between these facies belts is a...

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Figures & Tables

Contents

GeoRef

References

Related

Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal