Sociedad Geológica Mexicana, Boletín de la Sociedad Geológica Mexicana, 3(62), p. 305-323
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This paper describes the systematics of the main dating systems for geological and environmental processes during the late-Quaternary (<500000 years), specifically 14C, 210Pb, and 238U-234U-230Th. A short discussion is presented on the variety of samples amenable to dating, along with the advantages and limitations of the geochronological systems described here.