2018
DOI: 10.7546/crabs.2018.12.09
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New Data about the Dvoynitsa Formation Distribution in the Onshore Part of the Dolna Kamchiya Basin (Eastern Bulgaria) on the Base of 3D Lithological Modelling

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Cited by 4 publications
(4 citation statements)
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“…This study confirmed the various lithology of the Dvoynitsa Formation -three lithological types were recorded. Their complex spatial relationships, established in other parts of Eastern Balkanides (Vangelov, Sinnyovsky, 2011) and the Dolna Kamchia Basin (Valchev et al, 2018;Valchev, Dimitrov, 2019) were observed in the Solnik area, as well. The presence of two members (the Gebesh and Armera) was proved.…”
Section: Discussionmentioning
confidence: 82%
“…This study confirmed the various lithology of the Dvoynitsa Formation -three lithological types were recorded. Their complex spatial relationships, established in other parts of Eastern Balkanides (Vangelov, Sinnyovsky, 2011) and the Dolna Kamchia Basin (Valchev et al, 2018;Valchev, Dimitrov, 2019) were observed in the Solnik area, as well. The presence of two members (the Gebesh and Armera) was proved.…”
Section: Discussionmentioning
confidence: 82%
“…Recently, we established that, in the Dolna Kamchiya Basin, the Dvoynitsa Formation is composed of four lithological types (Valchev et al, 2018b): (i) clast-to matrix-supported conglomerates (sandy and clayey debrites); (ii) thick-bedded sandstones; (iii) rhythmic alternation of thin-bedded sandstones, marls and shales (thin-rhythmic turbidites); and (iv) brown-reddish and greenish clays and marls with thin interbeds of fine-grained sandstones. The former two lithological types were referred to the Armera Member, the third one to the Gebesh Member, and the latter one to the Goritsa Member.…”
Section: Dvoynitsa Formationmentioning
confidence: 99%
“…The former two lithological types were referred to the Armera Member, the third one to the Gebesh Member, and the latter one to the Goritsa Member. On the basis of planktonic foraminiferal data, we determined the chronostratigraphical range of the Dvoynitsa Formation as lower Ypresian-middle Lutetian (Valchev et al, 2018b). In the Eastern Balkanides, the unit ranges from the uppermost Maastrichtian to the middle Lutetian (Vangelov and Sinnyovsky, 2011).…”
Section: Dvoynitsa Formationmentioning
confidence: 99%
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