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Geochronological closure temperature

Scherer E. E., Cameron K. L., and Blichert-Toft J. (2000) Lu-Hf garnet geochronology closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions. Geochim. Cosmochim. Acta 64(19), 3413-3432. [Pg.1553]

Dodson, M. H. (1973). Closure temperature in cooling geochronological and petrological systems. Contrib. Mineral. Petrol., 40, 259-74. [Pg.529]

The concept of closure temperature is particularly important in geochronology. According to Dodson (1973), closure temperature f can be defined as the temperature of the system at the time corresponding to its apparent age. ... [Pg.738]

The analytical representation of closure temperature for a geochronological system (Dodson, 1973) is... [Pg.740]

Discrete values of closure temperatures in various minerals and mineral couples for the " °Ar- Ar and Rb-Sr geochronological systems are reported in table 11.5. [Pg.741]

A more direct approach to dating deformational features involves the application of isotopic geochronology to minerals that grew initially or were dynamically recrystallized during deformation at temperatures below their nominal closure temperatures (Reuter and Dallmeyer, 1989 Gromet, 1991 West and Lux, 1993 Coleman and Hodges, 1995 Resor et al., 1996 Dunlap, 1997 Anderson et al., 2001 Dallmeyer... [Pg.1542]

See other pages where Geochronological closure temperature is mentioned: [Pg.739]    [Pg.240]    [Pg.486]    [Pg.264]    [Pg.922]    [Pg.1541]    [Pg.1588]    [Pg.220]    [Pg.806]    [Pg.812]    [Pg.311]    [Pg.536]    [Pg.72]    [Pg.487]   
See also in sourсe #XX -- [ Pg.237 , Pg.238 , Pg.239 ]



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Closure temperature

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