Paleogeography and facies of the central and northeastern parts of the Moscow syneclise in the Devonian |
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Authors: | N K Andreeva N A Kagramanyan T N Kheraskova |
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Institution: | (1) Federal State Unitary Enterprise Research-Production Center for Superdeep Drilling and Comprehensive Study of the Earth’s Interior (Nedra), ul. Svobody 8/38, 150000 Yaroslavl, Russia;(2) Geological Institute (GIN), Russian Academy of Sciences, Pyzhevskii per. 7, 109017 Moscow, Russia |
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Abstract: | New data on the stratigraphy and composition of the Devonian rocks of the Moscow Syneclise were used. Facies-paleogeographic
schemes were compiled for the Lochkovian, Eifelian, Givetian, early-middle Frasnian, late Frasnian, and early-late Famennian
evolutionary stages of the Moscow Syneclise. Seven sedimentation cycles were developed due to sealevel fluctuations and structural
rearrangements in the paleooceanic basins surrounding the East European Platform at that time. The inference was made on the
structural heterogeneity of the platform basement and on differentiated movements as well as on the strike-slip fault nature
of some fragments of the basement relative to each other in the Devonian. |
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