Carbon dating absolute dating

24-Jan-2020 17:02

The basic principle Carbon has three naturally occurring (n is a neutron and p is a proton) After formation the three carbon isotopes combine with oxygen to form carbon dioxide.

U-Pb ages of zircon in sediments are used to determine the provenance of the sediments. Fission-track analysis is useful in determining the thermal history of a sample or region.

Quaternary geology provides a record of climate change and geologically recent changes in environment.

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