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- W1574504285 abstract "Publisher Summary This chapter focuses on the Yenisey fold belt. This belt is situated along the western edge of the ancient Siberian craton and most workers refer to it as the “Baikalides” or more recently as the “Ripheides.” Its area depends on whether or not the Angara–Kan micro-craton is included. Folded Riphean formations, which define all the belt's features, crop out mainly in the Trans-Angara part of the Yenisey ridge. An important factor in the creation of the belt structure is its situation in the collision zone between the Siberian craton and the West Siberian platform. The belt is characterized by territories that are highly differentiated on a number of counts: (1) the composition of the sedimentary and volcanosedimentary rocks, (2) their thickness, (3) deformation, and (4) the number and composition of volcanic and intrusive rocks. Depending on these characteristics, the Yenisey belt is divided into three main linear tectonic zones: (1) Eastern (Chernorechenko–Kamenskaya), (2) Central (Teysko–Tatar), and (3) Pre-Yenisey, which in turn are further divided into subzones." @default.
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- W1574504285 date "1997-01-01" @default.
- W1574504285 modified "2023-09-24" @default.
- W1574504285 title "Chapter 16 Yenisey fold belt" @default.
- W1574504285 doi "https://doi.org/10.1016/s0168-6178(97)80044-4" @default.
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