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Closure temperature in cooling geochronological and petrological systems

✍ Scribed by Martin H. Dodson


Publisher
Springer
Year
1973
Tongue
English
Weight
887 KB
Volume
40
Category
Article
ISSN
0010-7999

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Closure temperature (Tc) of a geochronological system may be defined as its temperature at the time corresponding to its apparent age. For thermally activated diffusion in which R is the gas constant, E the activation energy, z the time constant with which the diffusion coefficient D diminishes, a

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