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- W4242871330 abstract "Publisher SummaryThis chapter discusses cycles in the old red sandstone of Britain, molasse of Switzerland, flysch facies in molasse, Fluvio-Lacustrine coal-bearing sequences of Gondwanaland, and Witwatersrand system of South Africa. Deposits in fluvial regimes accumulate under different conditions, which can be regarded as variations between two extremes. Channels are continually choked with debris and the drainage deflected first one way and then another over the fan. Deposition is not over-rapid and the main changes are because of meandering of the channel, which carries different sediment types across the plain. While, there is therefore some doubt as to the importance of cyclicity in the sedimentation of the coal-bearing facies of the Beacon rocks, most authors seem to be in broad agreement as far as the environment of deposition is concerned. In general, from the Upper Carboniferous onwards, it appears that the temperature became less severe, as glacial conditions gave way to a more temperate climate, though the presence of coals may not imply warm-temperate or subtropical temperatures." @default.
- W4242871330 created "2022-05-12" @default.
- W4242871330 date "1967-01-01" @default.
- W4242871330 modified "2023-10-16" @default.
- W4242871330 title "Chapter 2 Cycles in Fluvial Regimes" @default.
- W4242871330 doi "https://doi.org/10.1016/s0070-4571(08)70122-5" @default.
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