A. W. McCrone; Thixotropy and the mobilization of clays in slumps and turbidity flows. Journal of Sedimentary Research ; 36 (1): 270. doi: https://doi.org/10.2110/jsr36.270
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Mobilization of clays in earthquake-triggered slumps and turbidity currents may be attributable to the thixotropic properties of the clays as well as to ordinary physical dislodgement.
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