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- W2034830149 abstract "Magnetic fabrics of weakly deformed rocks are not simply correlated with the principal finite strain directions. Depositional magnetic fabrics persist at 30% shortening where the rocks are deformed by particulate flow (grain boundary sliding). Rocks with a spaced, stylolitic cleavage (believed to be formed by “pressure solution”) and shortened by 20–50% have maximum susceptibility parallel to the intersection of cleavage and bedding. This type of magnetic fabric is attributed to the interference of a depositional magnetic fabric between cleavage surfaces with a tectonic magnetic fabric in the cleavage surfaces." @default.
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- W2034830149 date "1981-08-01" @default.
- W2034830149 modified "2023-10-07" @default.
- W2034830149 title "The influence of deformation mechanisms on magnetic fabrics in weakly deformed rocks" @default.
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- W2034830149 doi "https://doi.org/10.1016/0040-1951(81)90165-7" @default.
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