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Tephrocronologia×Datação por Luminescência Opticamente Estimulada×
ÁreaArqueologiaArqueologia
FamíliaProcess / pipelineProcess / pipeline
Ano de origem19441985
Autor originalSigurdur ThorarinssonDavid Huntley
TipoVolcanic marker dating techniqueLuminescence dating technique
Fonte seminalThorarinsson, S. (1944). Tefrokronologiska studier på Island. Geografiska Annaler, 26(1-2), 1-217. link ↗Huntley, D. J., Godfrey-Smith, D. I., & Thewalt, M. L. (1985). Thermoluminescence dating of ocean sediments. Canadian Journal of Earth Sciences, 22(3), 423-427. link ↗
Outros nomestephra chronology, volcanic ash datingOSL dating, optical dating
Relacionados44
ResumoTephrochronology is a chronometric and stratigraphic technique that uses volcanic ash layers (tephra) as time markers to date and correlate archaeological and geological deposits. Pioneered by Icelandic geologist Sigurdur Thorarinsson in 1944, it exploits the fact that large explosive volcanic eruptions deposit distinctive ash layers across vast geographic regions instantaneously in geological time. Each tephra layer serves as a chronological marker horizon that can be identified, characterized, and dated, enabling archaeologists to synchronize deposits across multiple sites.Optically stimulated luminescence (OSL) dating is a chronometric method that determines the age of sedimentary materials by measuring light-induced electron release from mineral grains. Developed by David Huntley and colleagues in the 1980s, it measures the time elapsed since sediment was last exposed to sunlight. This technique is widely used in archaeology, geology, and paleoenvironmental studies to date deposits ranging from a few decades to several hundred thousand years old.
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ScholarGateComparar métodos: Tephrochronology · Optically Stimulated Luminescence Dating. Recuperado em 2026-06-20 de https://scholargate.app/pt/compare