53 Cores and Rocks from the Southeast Atlantic Continental Margin to Facilitate Interstate Correlation of Along-Strike Units: A Hands-On Poster Session to Support Symposium 2 (Posters)

Tuesday, 16 April 2024
2:30 PM - 5:30 PM
Top of the Plaza

PLIOCENE AND EARLY PLEISTOCENE STRATIGRAPHIC UNITS IN THE DAUGHTRIDGE CORE OF NORTH CAROLINA: TO SUPPORT INTERSTATE CORRELATION OF FALL ZONE PLACER DEPOSITS

Paper number: 53-4
Program: Theme Sessions
Time: 2:30 PM – 5:30 PM

Authors

Abstract

The North Carolina Geological Survey (NCGS), the Virginia Dept. of Energy and federal scientists are collaborating to evaluate existing stratigraphic nomenclature and upgrade descriptions for surficial Pliocene and Pleistocene deposits that include heavy mineral placers in the Fall Zone of Virginia (VA) and North Carolina (NC). This effort is funded by USGS STATEMAP and EARTH MRI programs. NCGS drilled new core at 127 sites in Drake and Red Oak 7.5-minute quadrangles in NC including the Daughtridge core. In VA, mappers use traditional methods and an auger rig to map and define units. With STATEMAP funding for interstate correlation activities, NCGS drilled 367 ft of new core in VA in Dinwiddie and Cherry Hill 7.5-minute quadrangles at 13 sites along-strike.

To compare stratigraphy, core descriptions were standardized in graphic log format. Landscape positions were defined, and the logs with thick Coastal Plain units were chosen. In NC, the Daughtridge cores penetrated the Coharie terrace (150-246 ft; 45-75 m) between the Kenly and Wilson Mills paleoshorelines. In VA, the Clarke core cluster was situated on the Richmond Plain (205-240 ft; 62-73 m) between the Thornburg and Broadrock scarps in the Old Hickory heavy mineral deposit. All cores consist of 40 ft (12 m) of Coastal Plain section that overlies bedrock saprolite and occur at elevations of 200-217 ft (61-66 m). In VA, Clarke-03 was evaluated with a multi-sensor core logger system and sampled for cosmogenic nuclides. The units targeted may be the Cold Harbor (informal) and Bacons Castle Formations.

On display is the Daughtridge core which includes three sedimentary facies that are finer-grained than the Clarke core units: these form an upward coarsening succession of shelf, shoreface, foreshore and supratidal deposits. The basal unit (1 ft: 0.3 m) is a thin, burrowed, well-sorted very fine silty sand that sharply overlies saprolite. Unit 2 (19 ft: 5.8 m) has a basal gravel (1 ft: 0.3 m) that is sharply overlain by burrowed to laminated, very fine silty sands that coarsen upward into fine to medium heavy-mineral sands. Surficial Unit 3 has a lower part (4 ft: 1.3 m) consisting of feldspathic, slightly muddy and slightly gravelly coarse sand, with a basal gravel lag. Above this is a burrowed very muddy medium sand and sandy mud with plinthite nodules and quartz pebbles (12 ft; 3.6 m).

Geological Society of America Abstracts with Programs. Vol. 56, No. 2

doi: 10.1130/abs/2024SE-398307

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