Thermoluminescence dating of ancient ceramics
Creators
- 1. Research Laboratory for Archaeology and the History of Art, University of Oxford (United Kingdom)
Description
Absolute dating by the thermoluminescence technique, rather than the relative dating previously aimed for, is possible if allowance is made for radiation attenuation effects. To do this the thermoluminescence measurements are made on crystalline inclusions separated out from the fine-grained clay matrix. These inclusions, which are usually quartz, are large enough for their average radiation dose from alpha particles originating in the clay matrix to be negligible. Since the uranium and thorium are carried predominantly in the clay matrix, the natural thermoluminescence acquired by the inclusions comes effectively only from the beta and gamma contributions. A preliminary test programme on known-age pottery fragments dating back to 8000 B. P. has given correct absolute ages to within ± 20%. (author)
Additional details
Publishing Information
- Publisher
- IAEA
- Imprint Place
- Vienna (Austria)
- Imprint Title
- Radioactive dating and methods of low-level counting. Proceedings of a symposium
- Imprint Pagination
- 744 p.
- Series
- Proceedings series
- Journal Page Range
- p. 523-530
- ISSN
- 0074-1884
Conference
- Title
- Symposium on radioactive dating and methods of low-level counting
- Dates
- 2-10 Mar 1967
- Place
- Monaco (Monaco)
INIS
- Country of Publication
- Austria
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 38058855
- Subject category
- S58: GEOSCIENCES;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- ALPHA PARTICLES; ATTENUATION; CERAMICS; CLAYS; ISOTOPE DATING; QUARTZ; RADIATION DOSES; THERMOLUMINESCENCE; THORIUM; URANIUM
- Descriptors DEC
- ACTINIDES; AGE ESTIMATION; CHARGED PARTICLES; DOSES; ELEMENTS; EMISSION; IONIZING RADIATIONS; LUMINESCENCE; METALS; MINERALS; OXIDE MINERALS; PHOTON EMISSION; RADIATIONS; SILICATE MINERALS
Optional Information
- Notes
- 14 refs, 4 figs, 3 tabs
- Secondary number(s)
- IAEA-SM--87/37