Journal
RUSSIAN JOURNAL OF PACIFIC GEOLOGY
Volume 11, Issue 6, Pages 383-394Publisher
MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S1819714017060069
Keywords
stratigraphy; tectono-stratigraphic systems; paleogeography; paleogeodynamics; Mesozoic; Uda and Torom sedimentary basins; Far East of Russia
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Funding
- Far East Program of Fundamental Research of the Far East Branch, Russian Academy of Sciences [15-I-2027, 15-1-2-030]
- Russian Foundation for Basic Research [16-05-00571/16]
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The stratigraphic succession of the Mesozoic suites in the Uda and Torom sedimentary basins and the hiatuses and unconformities in the section and their duration are analyzed. The tectono-stratigraphic systems are distinguished with respect to the regional and global geological events, which makes it possible to trace the evolution of these fragments in the continental margin in the Mesozoic, as well as to propose paleogeographic and paleogeodynamic reconstructions.
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