Thermoluminescence Dating
Thermoluminescence (TL) dating is a chronometric technique that determines the age of pottery, ceramics, and sediments by measuring light emitted when heated to high temperatures. Pioneered by Michael Aitken in the 1960s, it quantifies the accumulated radiation dose stored in mineral crystal lattices. The method revolutionized archaeological dating by enabling scientists to date ceramic vessels and fired clay objects directly, providing absolute chronologies for human occupation sites worldwide.
Source record
Citations copied verbatim from the method’s source record. No claim-level verification is inferred from them.
- Aitken, M. J. (1985). Thermoluminescence Dating. Academic Press. · URL
- Prescott, J. R., & Hutton, J. T. (1994). Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations. Radiation Measurements, 23(2-3), 497-500. · DOI 10.1016/1350-4487(94)90086-8
- Wintle, A. G. (2005). Luminescence dating: laboratory procedures and protocols. Radiation Measurements, 27(5-6), 769-817. · URL
Curated claims
Claims persisted in the evidence ledger, each with its own assessment.
This view does not invent a claim assessment when the ledger has none.
Related methods
Generated from the method graph and shown as machine-suggested relations — no evidence claim is inferred.