A5013089830- Geological Studies and Exploration
- Paleontology and Stratigraphy of Fossils
- Marine and environmental studies
- Geological and Geochemical Analysis
- Hydrocarbon exploration and reservoir analysis
- Geology and Paleoclimatology Research
- Geochemistry and Geologic Mapping
- Geological Formations and Processes Exploration
- Methane Hydrates and Related Phenomena
- Marine Biology and Ecology Research
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Paleontology and Evolutionary Biology
- Geological formations and processes
- Ancient and Medieval Archaeology Studies
- Astro and Planetary Science
- Archaeology and ancient environmental studies
- Aging, Elder Care, and Social Issues
- High-pressure geophysics and materials
- Linguistics and language evolution
- Hydraulic Fracturing and Reservoir Analysis
- French Urban and Social Studies
- Social Sciences and Governance
- Soil and Environmental Studies
- Evolution and Paleontology Studies
Moscow State University
2008-2024
Lomonosov Moscow State University
2015-2024
University of Warsaw
2015
Russian Academy of Sciences
2014
Abstract We provide a synthesis of stratigraphic data to unravel the history geological evolution South Crimea in Mesozoic and Cenozoic. The Orogen consists three major mega-sequences: (1) Triassic–Early Jurassic; (2) Aalenian–Bathonian; (3) Callovian–Eocene. Late Jurassic deposits formed environment forearc basin remnant basin. Aalenian–Bathonian above subduction extension volcanic belt. Three main Callovian–Eocene tectonic units can be identified Crimea: Crimean Shelf Basin; Sudak...
ABSTRACT Walaszczyk, I., Kopaevich, L.F. and Beniamovski, V.N. 2013. Inoceramid foraminiferal record biozonation of the Turonian Coniacian (Upper Cretaceous) Mangyshlak Mts., western Kazakhstan. Acta Geologica Polonica, 63 (4), 469-487. Warszawa. The Kazakhstan, yielded a rich relatively complete inoceramid bivalve record. faunas their succession correspond to those known from central eastern Europe, allowing zonation established in latter areas be applied virtually identical form. gaps...
Abstract The main palaeogeographic features of the Late Cretaceous Eastern European Platform and its southern framework are reconstructed mainly based on micropalaeontological data. An integrated foraminiferal–radiolarian zonation for Upper Albian–Maastrichtian serves as a basis reconstructions interpretation palaeoclimate sea-level trends. study focuses time slices late Albian–Cenomanian, Turonian–Coniacian Santonian–Campanian intervals. Albian was characterized by gradual disappearance...