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- W1554920302 abstract "Paleontologic studies of DSDP Leg 96 cores support several mechanisms for deposition of Quaternary sediments on the Mississippi Fan: 1) density flow, 2) debris flow, and 3) suspension load. The constituents of the faunal assemblages suggest that the sediments were derived from: 1)upper Mississippi Valley—reworked Cretaceous foraminifers and radiolarians, 2)Louisiana continental shelf—displaced shallow water benthic foraminifers, and3Florida continental shelf—displaced carbonate bank assemblage. Calculated sedimentation rates for the fan are 2 to 13 cm/1000 yr for the Holocene, 600 to 1100 cm/1000 yr for the late Wisconsin glacial, and 71 cm/1000 yr for the Wisconsin interstadial." @default.
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- W1554920302 date "1985-01-01" @default.
- W1554920302 modified "2023-10-03" @default.
- W1554920302 title "Biostratigraphy and Sedimentation Rates of the Mississippi Fan" @default.
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- W1554920302 doi "https://doi.org/10.1007/978-1-4612-5114-9_39" @default.
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