Thermoluminescence dating of soils in a semi-arid environment, Yucca Mountain area, Southern Nevada, USA
Yucca Mountain, Nevada, is currently being investigated as a potential nuclear waste repository. Because radionuclides must be isolated over a ten to several hundred thousand year time span, an assessment of the performance depends in part on accurate reconstruction of the Quaternary geologic and hydrologic history of the mountain. Reliable geochronology in an oxidizing environment dominated by coarse-grained, clastic surficial deposits has become a central issue for several studies including paleoseismic reconstruction, determination of rates of erosion and deposition, and the history of regional water-table fluctuations documented by ground-water discharge deposits. Thermoluminescence (TL) dating of polymineralic silt fractions in a variety of surface deposits has become an important component of the Quaternary dating strategy, along with uranium-series disequilibrium dating of secondary carbonate and opaline silica, and to a lesser extent, radiocarbon dating of carbonate components. Although the complex mineralogy of these materials contributes to greater amounts of scatter in their TL response relative to typical quartzofeldspathic loess and dune deposits, the derived ages are reproducible, consistent with internal stratigraphy, and generally concordant with other available geochronology.
- Research Organization:
- US Geological Survey, Denver, CO (United States)
- Sponsoring Organization:
- USDOE, Washington, DC (United States)
- DOE Contract Number:
- AI08-92NV10874
- OSTI ID:
- 231941
- Report Number(s):
- CONF-951279-1; ON: DE96009869; TRN: 96:012799
- Resource Relation:
- Conference: Luminescence and ESR research seminar, Sussex (United Kingdom), 19-20 Dec 1995; Other Information: PBD: 1995
- Country of Publication:
- United States
- Language:
- English
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