Σύγκριση μεθόδων

	Χρονολόγηση Ουρανίου-Θορίου	Χρονολόγηση με Ηλεκτρονικό Συντονισμό Σπιν
Πεδίο	Αρχαιολογία	Αρχαιολογία
Οικογένεια	Process / pipeline	Process / pipeline
Έτος προέλευσης	1955	1980s
Δημιουργός	Harmon Craig	Michael Aitken
Τύπος	Decay series dating technique	Paramagnetic resonance dating technique
Θεμελιώδης πηγή	Edwards, R. L., Chen, J. H., & Wasserburg, G. J. (1987). U-238, U-234 and Th-230 in seawater. Geochimica et Cosmochimica Acta, 51(5), 1213-1225.	Grün, R. (1989). Electron spin resonance (ESR) dating. Quaternary International, 1, 65-109.
Εναλλακτικές ονομασίες	U-Th dating, thorium-230 dating	ESR dating, electron paramagnetic resonance dating, EPR dating
Συναφείς	4	4
Σύνοψη	Uranium-thorium (U-Th) dating is a chronometric method that determines the age of carbonates, shells, bones, and coral by measuring the ratio of uranium isotopes to thorium-230. First applied by Harmon Craig in the 1950s, it exploits the natural radioactive decay chain of uranium. U-Th dating is particularly valuable for dating materials from 500 to 500,000 years old, filling a crucial chronological gap between radiocarbon and potassium-argon dating.	Electron spin resonance (ESR) dating is a chronometric method that determines the age of bones, teeth, mollusk shells, and sediments by measuring accumulated radiation-induced unpaired electrons. Developed by Michael Aitken in the 1980s, ESR detects free radicals trapped in mineral crystal structures. Unlike luminescence techniques that require heating or light exposure, ESR directly measures paramagnetic defects, making it particularly valuable for dating dental and skeletal remains that are inaccessible to other methods.