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https://doi.org/10.1306/74d70484-2b21-11d7-8648000102c1865d
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Cite Journal: SEPM Journal of Sedimentary Research |  Publication Date: Jan 1, 1955 |
Physical features of the fucoidal markings in the Swan Peak formation suggest a mode of origin involving incorporation of coarse sand particles and organic fragments in a gelatinous organism plus the influence of the chemical by-products of the decomposition of the organism on the cementation process during diagenesis.
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