Abstract
The principal primary and secondary structures are 1) homogeneous bedding, 2) composite bedding, 3) graded bedding, 4) parallel lamination, 5) cross-lamination, 6) discontinuous and irregular structures, and 7) microfaults and loading structures. Most of these structures, and their common occurrence in regular vertical successions over 5 to >100 cm, can be interpreted in terms of the standard sequences for fine-grained turbidites. However, several other structures are most likely the result of particularly rapid deposition from large muddy turbidity currents onto a soft, unconsolidated substrate. -from Authors
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CITATION STYLE
Cremer, M., & Stow, D. A. V. (1986). Sedimentary structures of fine-grained sediments from the Mississippi Fan: thin-section analysis. Initial Reports DSDP, Leg 96, Ft. Lauderdale to Galveston, Texas, 1983, 519–532. https://doi.org/10.2973/dsdp.proc.96.124.1986
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