2019
DOI: 10.7306/gq.1452
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Turonian–Coniacian (Upper Cretaceous) of the Babadag Basin (North Dobrogea, Romania): integrated biostratigraphy and microfacies succession

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“…1a). The NDO experienced an extensional tectonic regime from the Early Triassic to the mid-Carnian and started to be inverted and telescoped by thrusting during the early Mesozoic Cimmerian orogeny and ending during the mid-Cretaceous Alpine tectonogenesis, being overstepped by the Vraconian-Late Cretaceous sedimentary series of the post-tectonic Babadag Basin (Mirăuţă & Mirăuţă 1964;Burchfiel & Bleahu 1976;Grădinaru 1995Grădinaru , 2004Grădinaru , 2006Lodowski et al 2019).…”
Section: Geological Settingmentioning
confidence: 99%
“…1a). The NDO experienced an extensional tectonic regime from the Early Triassic to the mid-Carnian and started to be inverted and telescoped by thrusting during the early Mesozoic Cimmerian orogeny and ending during the mid-Cretaceous Alpine tectonogenesis, being overstepped by the Vraconian-Late Cretaceous sedimentary series of the post-tectonic Babadag Basin (Mirăuţă & Mirăuţă 1964;Burchfiel & Bleahu 1976;Grădinaru 1995Grădinaru , 2004Grădinaru , 2006Lodowski et al 2019).…”
Section: Geological Settingmentioning
confidence: 99%