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- W2280690802 abstract "Convergent motion of the North American and Juan de Fuca plates has resulted in deformation of Cascadia Basin sediments and accretion of these deposits to. the Washington-Oregon (lower) continental slope. , Nearsurface accreted deposits consist largely of'Pleistocene/ Pliocene mudstones, which have undergone mechanical consolidation. Some of th-e,se deposits exhibit a rudimentary spaced cleavage.^ The foliation is^inclined*approximately 80° to bedding. Individual folia are typically spaced 1.5 to 2.0 mm apart, although the spacing varies from 0.5 to 10 mm. Observation by scanning electron and optical microscopy reveal the folia to be zones o-f.. sub parallel phyllosilicate (clay) flakes. These zones range in width from 10jum to 150 p.m, are at least 10 cm long, and commonly anastomose. Along the edges of the folia, grains with an orientation intermediate between bedding and foliation are observed. Disaggregated deep sea mudstone artificially,, deformed (total strain = -0.17; strain rate = 1.1 x -7 -1 10 ' s ) in the laboratory also exhibits water loss (initial water content<90 percent dry weight, final _ water content «*60 to 87 percent). The fabric resulting^" @default.
- W2280690802 created "2016-06-24" @default.
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- W2280690802 date "1980-01-01" @default.
- W2280690802 modified "2023-09-26" @default.
- W2280690802 title "Phyllosilicate fabric in naturally deformed mudstone from the Washington continental slope and comparison with experimentally induced fabric." @default.
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