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- W2049259104 abstract "A few different wasy of formation of diamictons that to some extent could be considered till are discussed. Shearing, brecciation and flow as a result of glacier action deformed and mixed waterlaid sediments to become diamictons. The structures observed illustrate the ways of formation. Similar structures found in e.g., Precambrian sediments could be an indication of glacial deformation." @default.
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- W2049259104 date "1985-10-01" @default.
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- W2049259104 title "Glaciotectonic and till or tillite genesis: Examples from pleistocene glacial drift in central Sweden" @default.
- W2049259104 cites W2042602488 @default.
- W2049259104 doi "https://doi.org/10.1016/0031-0182(85)90095-1" @default.
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