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Stratigraphy, depositional rates, and other DSDP Leg 96 conclusions: Mississippi fan

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6608826

The Quaternary Mississippi fan consists of at least seven seismically mappable fan lobes. Eight sites were drilled into the youngest fan lobe during DSDP Leg 96. The Holocene (Ericson Zone Z) is capped by a marly foraminiferal ooze. Assuming an age of 12,000 yr for the Holocene/Pleistocene boundary, a minimum accumulation rate of 3-30 cm/1000 yr (1-12 in/1000 yr) is computed for the Holocene. The youngest fan lobe was deposited during the upper part of Ericson Zone Y (late Wisconsin glacial, 12,000-85,000 y.B.P.). Deposition rates for the Y Zone are extremely high for the middle fan sites, averaging 12 m/1000 yr (39 ft/1000 yr). Lower fan accumulation rates are 7 m/1000 yr (23 ft/1000 yr) for the channel sites and 6 m/1000 yr (20 ft/1000 yr) for the channel-mouth depositional lobes. These rates are not corrected for compaction. Foraminifera are scarce; the occurrence of shallow-water benthic species indicates a displaced inner and middle neritic origin for the sediments. Drilling on the youngest fan lobe shows that most of the silts and sands were transported through the upper and middle fan channel onto the lower fan, producing a 6 to 10-km (4 to 6-mi) wide, 135-m (443-ft) thick aggradational channel deposit. Much of the fine-grained sediment spilled out of the channel onto the adjacent overbank areas, constructing broad marginal plain. The channels on the lower fans are smaller and shift position frequently. Channel-mount depositional lobes are constructed at the end of the active channels and are composed of more than 50% net sand.

Research Organization:
Louisiana State Univ., Baton Rouge
OSTI ID:
6608826
Report Number(s):
CONF-8405216-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Vol. 68:4; ISSN AAPGB
Country of Publication:
United States
Language:
English