Helium diffusion from apatite: General behavior as illustrated by Durango fluorapatite

By K. Farley. 2000

1,027 citations recorded by the source corpus.

Subfields: Geophysics, Materials Chemistry

View Paper: https://www.semanticscholar.org/paper/5f5d4ff3d8392aeba344f2395a525bec1d5349e2

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Citations in the corpus

The influence of artificial radiation damage and thermal annealing on helium diffusion kinetics in apatite (2009, background): “of Fechtig and Kalbitzer (1966) for diffusion kinetics determined from stepwise release fractions of proton-induced (3)He or natural radiogenic (4)He.”
Past, Present, and Future of Thermochronology (2005, background): “…as yet poorly understood aspects of He diffusion that may have broader implications are crystallographic anisotropy in diffusion characteristics (Farley 2000), and the fact that 3He and 4He appear to diffuse from apatite at essentially the same rate (Shuster et al. 2003), rather than with the…”
Transdimensional inverse thermal history modeling for quantitative thermochronology (2012, neutral): “…domains, either within single crystals (40Ar/39Ar method) [McDougall and Harrison, 1999] or multiple grains (Helium method) as the grain is generally considered to be the diffusion domain for apatite [Farley, 2000, Reiners and Farley, 2001] and also probably for zircon [Reiners et al., 2004].”
Effect of alpha-damage annealing on apatite (U–Th)/He thermochronology (2009, methodology): “Therefore, a realistic description of the time evolution of α-recoil damage has become essential for (U–Th)/He thermochronology, as shown also by the recent and similar study from Flowers et al. (2009). Similarly to Farley (2000) and Shuster et al.”
The influence of natural radiation damage on helium diffusion kinetics in apatite (2006, methodology): “Since helium diffusion in apatite is nearly isotropic [3], isolated damage cascades may provide enough space between displaced atoms where (4)He atoms may accumulate at a lower energy state.”
Helium diffusion in natural zircon: Radiation damage, anisotropy, and the interpretation of zircon (U-Th)/He thermochronology (2013, background): “…or ones similar to it, has been observed previously in zircon (Reiners and others, 2002; Reiners and others, 2004) and several other minerals, including titanite (Reiners and Farley, 1999), goethite (Shuster and others, 2005), magnetite (Blackburn and others, 2007), and apatite (Farley, 2000).”
Crustal Thermal Processes and the Interpretation of Thermochronometer Data (2005, background): “Thus, quantifying changes in thermal gradients is a necessary step to quantifying changes in cooling rates and calculation of cooling rate dependent closure temperatures (e.g., Dodson 1973,1986; Farley 2000).”
Pecube: a new finite-element code to solve the 3D heat transport equation including the effects of a time-varying, finite amplitude surface topography (2003, methodology): “From these T � t paths, an apparent (U–Th)/He age for apatite can be computed at each location, following the procedure and parameter values given by Wolf et al. (1998) and Farley (2000) .”