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- W1970000003 abstract "The production of narrow shear zones was recently shown to be the chief mechanism by which wet argillaceous sediments deform in the laboratory. This article illustrates, by considering a variety of circumstances in which sediments deform, that this mode of deformation is of widespread importance in nature. Examples are given of shear zones, highly similar to the experimentally produced features, in glaciogenic sediments and D.S.D.P. cores; and in deformed sediments that are now lithified. The latter examples include the results of both gravitationally-induced disturbances such as slumping, and possible tectonically-formed features such as occur in accretionary complexes. Implications of recognizing the natural shear zones are mentioned, for example, their influence on dewatering behaviour, their possible use as shear-sense indicators, and the possibility that they may indicate the physical conditions of the sediment deformation." @default.
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- W1970000003 date "1988-01-01" @default.
- W1970000003 modified "2023-09-27" @default.
- W1970000003 title "The importance of shear zones in naturally deformed wet sediments" @default.
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- W1970000003 doi "https://doi.org/10.1016/0040-1951(88)90324-1" @default.
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