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Geochronology is the study to determine the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves. Absolute geochronology can be accomplished through radioactive isotopes, whereas relative geochronology is determined by tools such as palaeomagnetism and stable isotope ratios.
Related Journals of Geochronology
Geology & Earth science, Geophysics Research Letters, Geology, Paleogeography and Paleoclimatology, Norwegian Journal of Geology, Journal of Iberian Geology, Journal of the Geological Society of Japan, Andean Geology, GeoScience Engineering, Annals of Geophysics, Contemporary Trends in Geoscience and Journal of Geological Research.