Variability of deltaic sedimentation during clastic influx into a carbonate-dominated craton
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6458481
Depositional styles of cratonic deltas vary significantly over short lateral distances. Sediment yield and water depths of the receiving basin are the determinant factors (in addition to fluvial, tidal, and wave action) that control cratonic deltaic variability associated with rapid progradation, particularly in the Hardinsburg Sandstone (Upper Mississippian) of the Illinois Basin. The Hardinsburg Sandstone consists of a lower, thin prodelta mudstone, a middle, thick fluvial - tidal flat - shoreface sandstone, and an upper, thick overbank - crevasse splay - interdistributary bay mudstone. Hardinsburg sandy cross-bedded fluvial channels prograded rapidly toward the Southwest into a tidally-influenced shallow shelf and eroded lower prodelta mudstones and underlying carbonates. Prodelta and delta front sediments were preserved best in regions flanking channel sandstones, with the thickest, most complete sequences being preserved in slightly deeper shelf areas. Shallow water distributary point bars formed widespread sand sheets which were reworked in interchannel regions both by Eastward-flowing longshore currents and by Northeast-Southwest oriented tidal currents. Rapid fluvial-deltaic Southerly progradation from the deeper basin center to the shallower Southern basin rim resulted in a shift from storm and wave influenced parallel-bedded sandy shelves to tidally-influenced rippled and flaser bedded sandstone shelves. Because sediment yield was insufficient to stabalize depositional environments over broad areas for long periods, cyclothems did not form. Subsidence of delta marsh and interdistributary muds and cessation of terrigenous influx favored marine transgression and a return to carbonate deposition.
- Research Organization:
- Geology Dept. Urbana, IL (USA)
- OSTI ID:
- 6458481
- Report Number(s):
- CONF-8510489-
- Conference Information:
- Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
- Country of Publication:
- United States
- Language:
- English
Similar Records
Deltaic sedimentation and transgressive/regressive cycles in Green River Formation, southern Uinta basin, Utah
Estuarine sandstones in Lower Pennsylvanian strata in the Indiana portion of the Illinois basin
Depositional environments of a reservoir sandstone in west-central Texas
Conference
·
Tue Feb 28 23:00:00 EST 1989
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:6132566
Estuarine sandstones in Lower Pennsylvanian strata in the Indiana portion of the Illinois basin
Conference
·
Thu Feb 28 23:00:00 EST 1991
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:5675675
Depositional environments of a reservoir sandstone in west-central Texas
Journal Article
·
Mon Feb 28 23:00:00 EST 1977
· Am. Assoc. Pet. Geol. Bull.; (United States)
·
OSTI ID:7322113
Related Subjects
58 GEOSCIENCES
580100* -- Geology & Hydrology-- (-1989)
COASTAL REGIONS
DEPOSITION
FEDERAL REGION IV
FEDERAL REGION V
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
GEOLOGY
ILLINOIS
ILLINOIS BASIN
INDIANA
KENTUCKY
LITHOLOGY
MISSISSIPPIAN PERIOD
NORTH AMERICA
PALEOZOIC ERA
RIVER DELTAS
RIVERS
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEDIMENTATION
SEDIMENTS
STRATIGRAPHY
STREAMS
SURFACE WATERS
USA
VARIATIONS
580100* -- Geology & Hydrology-- (-1989)
COASTAL REGIONS
DEPOSITION
FEDERAL REGION IV
FEDERAL REGION V
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
GEOLOGY
ILLINOIS
ILLINOIS BASIN
INDIANA
KENTUCKY
LITHOLOGY
MISSISSIPPIAN PERIOD
NORTH AMERICA
PALEOZOIC ERA
RIVER DELTAS
RIVERS
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEDIMENTATION
SEDIMENTS
STRATIGRAPHY
STREAMS
SURFACE WATERS
USA
VARIATIONS