作者: Alexander S. Alekseev , Lyudmila I. Kononova , Anatoly M. Nikishin
DOI: 10.1016/S0040-1951(96)00229-6
关键词:
摘要: Abstract The Moscow Syneclise is a vast sedimentary basin located in the centre of East-European Platform. Palaeozoic sequence this syneclise, and especially its Devonian-Carboniferous part, most suitable for sea-level fluctuation analysis. Devonian Carboniferous sediments consist mainly shallow-marine carbonates, containing several minor terrigenous intervals; they attain total thicknesses up to 1.5 km. modern stratigraphic scale includes 33 regional stages 32 Carboniferous. Correlation with global scales supported by conodont, miospore foraminifera zonations. new calibrated relative curves reflect late Eifelian, mid-Frasnian, early Tournaisian, Visean-early Serpukhovian Moscovian-Gzhelian transgressions. Several these changes, which are particularly evident on margins Syneclise, originated response differential tectonic movements Voronezh Anteclise Tokmovo Uplift as well vertical oscillations entire craton.