9 Undergraduate Research (Posters)
Thursday, 7 April 2022
8:00 AM - 12:00 PM
Junior Ballroom B
SPECTRAL GAMMA RAY RESPONSE IN A MIXED CARBONATE-SILICICLASTIC CHANNEL SYSTEM, FORT PAYNE (MIDDLE MISSISSIPPIAN), TENNESSEE
Paper number: 9-5
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Jeannette Wolak LunaTennessee Tech University, Cookeville, TN
Abstract
The research was conducted on an outcrop on TN Highway 52 (36°30’11.97”N, 85°26’49.62”W), three miles east of Celina, Tennessee. Here, the Fort Payne Formation is characterized by interbedded crinoidal packstones, grainstones, and siliciclastic shales. These lithologies fill a submarine channel incised into micritic and siliciclastic mudstone.
Scintillometer measurements were collected on a 10x10m grid at the base of the channel. A total of 100 data points were collected at 20 cm increments, comparable to downhole wireline log spacing but including a lateral as well as vertical (grid) component. A Gamma Surveyor II was used to measure potassium (%), thorium (ppm), uranium (ppm) and a general measurement of gamma radiation dose rate. Preliminary results suggest that the margins of submarine channels in the Fort Payne Formation are only resolvable where channel fill includes a siliciclastic shale component. In cases where channels incise similar lithologies it is not possible to use wireline logs to resolve submarine architectural elements.
Geological Society of America Abstracts with Programs. Vol. 54, No. 4
doi: 10.1130/abs/2022NC-375024
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