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Now showing items 1-7 of 7
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(1992)A global shift in carbonate carbon δ13C-values from heavier values in the Maastrichtian to lighter values in the early Danian indicates recycling of isotopically light organic carbon to inorganic carbon reservoirs during ...
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(1997)It has been established that every tenth bed of the Upper Cretaceous-Danian flysch deposits can be traced along the southern slope of the Greater Caucasus over a distance of 1035 km. This allowed 196 synchronous markers ...
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(1989)The Khatyr Basin, located in the eastern part of the Koryak highland, is bordered on the northwest by Cenozoic fold structures and opens to the southeast into the Aleutian Basin of the Bering Sea. The present study discusses ...
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(1989)Detailed stratigraphic schemes of the Upper Cretaceous sediments in the Caucasus allowed us to identify the presence of hiatuses and intraformational erosion surfaces based on the omission of one or another stratigraphic ...
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(1996)The vertical distribution of macrofossils (echinoids, biyozoans, brachiopods, bivalves, and others), and planktonic and benthic foraminifers was studied in several Paleocene and Eocene sections of western Mangyshlak. The ...
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(2006)The sediment composition and sedimentation conditions of Maastrichtian and Danian deposits in the vast territory of the Russian plate and adjacent regions of North Eurasia were studied. The succession of Late Cretaceous ...
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(1997)Representatives of the genus Danocrania Rosenkrantz 1964 from the Danian stage in the Crimea are presented, and the distinguishing features of this genus are described. Seven morphological types of brachiopods belonging ...
Now showing items 1-7 of 7