This paper presents the preliminary results of the biostratigraphic and microfacial study of Guri e Pellumbit section, in Klos region (Mirdita area. Benthic foraminifera and “microproblematica” are the main components of Lower Cretaceous reefs and carbonate platforms and have proved to be extremely helpful in the zonation of platform carbonates. The mixture of typical elements of shallow water environments (foraminifera, calcareous algae and microproblemica) with elements of deep environments (calpionellids) and the specific microfacies described in this study are typical for an allodapic limestones (turbidites). Based on the micropaleontological associations with biostratigraphical importance, the age of these deposits is Upper Beriassian-Lower Valanginian.
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Primary Language | English |
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Subjects | General Geology |
Journal Section | Articles |
Authors | |
Publication Date | June 30, 2019 |
Acceptance Date | June 14, 2020 |
Published in Issue | Year 2020 Volume: 15 Issue: 2 |
“Journal of International Environmental Application and Science”