A. I. Rees; The magnetic fabric of a sedimentary rock deposited on a slope. Journal of Sedimentary Research ; 41 (1): 307–309. doi: https://doi.org/10.1306/74D72257-2B21-11D7-8648000102C1865D
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The magnetic fabric of a convoluted sandstone is simple despite the complex deformation of the sedimentary structures. This is thought to be due to local fluidization of the sediment during deformation.
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