2017
DOI: 10.1007/s10347-017-0499-7
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The Cenomanian–Turonian boundary in the northwestern part of the Adriatic Carbonate Platform (Ćićarija Mtn., Istria, Croatia): characteristics and implications

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Cited by 14 publications
(10 citation statements)
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“…This facies is very similar and probably correlates with the coeval Sveti Duh Fm, outcropping some 80 km to the southeast in Istria and Dalmatia (e.g. Brčić et al, 2017, see Fig. 1).…”
Section: Casso Section Lithostratigraphymentioning
confidence: 59%
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“…This facies is very similar and probably correlates with the coeval Sveti Duh Fm, outcropping some 80 km to the southeast in Istria and Dalmatia (e.g. Brčić et al, 2017, see Fig. 1).…”
Section: Casso Section Lithostratigraphymentioning
confidence: 59%
“…In fact, toward the east in Istria and south of it (see Fig. 1), the east-dipping Cenomanian ramp was characterized by partial drowning, with pelagic limestones rich in open-sea organisms (Gušić and Jelaska, 1993;Korbar et al, 2012;Brčić et al, 2017). These facies, started around the early-middle Cenomanian, reached the maximum diffusion at the Cenomanian/Turonian boundary, which may be seen as the effect of OAE 2 and related sea-level rise on the platform margin.…”
Section: Accepted Manuscriptmentioning
confidence: 94%
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