History of geologic development of the Belbek-Kachinsky interfluve of the mountainous Crimea in the late Valanginian-Albian ages of the Early Cretaceous
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Abstract
The complexity of the geological development of the Earth's crust within the Mountain Crimea during the Jurassic and Cretaceous periods has been repeatedly noted in the geological literature. In the Belbek-Kachinsky interfluve, the Early Cretaceous history is quite clearly traceable to the end of the Valanginian; the geologic events of the end of the Early Cretaceous are less clearly delineated because of the incompleteness of the stratigraphic section ...
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References
- Gorbachik T.N., Drushchits V. V., Yanin B.T. Lower Cretaceous sediments of the Belbek-Alma interfluve (Crimea). - MSU Bulletin, Ser. Geol. 1975, No. 6, pp. 19-30.
- Kravtsov A.G., Shalimov A.I. Stratigraphy of Lower Cretaceous sediments in the basin of the middle course of the Belbek River (southwestern Crimea). – University Proc. Geology and Exploration, 1978, No. 9, p. 43-53.
- Muratov M.V. Tectonics and History of Development of the Alpine Geosynclinal Region of the South of the European Part of the USSR and Adjacent Countries. Tectonics of the USSR. V. 2, M.-L., PH of the USSR Academy of Sciences, 1949, 510 p.
- Muratov M.V. Brief sketch of the geologic structure of the Crimean Peninsula. Moscow, Gosgeoltekhizdat, 1960, 207 p.
- Odessky I. A. Morphometric analysis of the Lower Cretaceous conglomerates of the Crimea. - Lithology and Mineral Resources, 1969, No. 1, pp. 146-152.
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