Pb diffusion in rutile

By D. Cherniak. 2000

305 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Geochemistry and Petrology, Geophysics

View Paper: https://www.semanticscholar.org/paper/855e4768595a8596e1ca64c45ccbaeb9135888b6

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

1. J. E. Manchester
2. E. Bruce Watson
3. D. Cherniak
4. S. Bowring
5. B. Schoene

In Geochemistry and Petrology

1. J. E. Manchester
2. E. Bruce Watson
3. D. Cherniak
4. S. Bowring
5. B. Schoene

In Geophysics

1. S. Bowring
2. B. Schoene
3. J. E. Manchester
4. E. Bruce Watson
5. D. Cherniak
6. Roger S. Powell
7. David Ellis
8. H. Tomkins

Citations in the corpus

• Zr and Hf diffusion in rutile (2007, methodology): “Also plotted for comparison is a curve for Pb in rutile, generated with the diffusion parameters from Cherniak (2000). At temperatures above∼600 °C, Zr signatures in rutile are more likely to be retained than Pb isotope signatures.”
• Temperature dependence of Zr in rutile: empirical calibration of a rutile thermometer (2004, background): “Cherniak (2000) . It is shown that Zr diffusion in rutile (data from Sasaki et al. 1985) is similar to that of Pb. Diffusional resetting of Zr in rutile during cooling is therefore possible down to the closure temperature for the Pb system, which has been given as ca. 635� C (cooling rate 1� C/Ma, 2”
• U–Pb systematics of the McClure Mountain syenite: thermochronological constraints on the age of the 40Ar/39Ar standard MMhb (2006, background): “In addition, minerals with lower Tc such as titanite (Tc550–650� C; Cherniak 1993; Corfu 1988; Frost et al. 2000), apatite (Tc450–550� C; Chamberlain and Bowring 2000; Cherniak et al. 1991; Nemchin and Pidgeon 1999) and rutile (Tc400–500� C; Cherniak and Watson 2000; Mezger et al. 1991; Schmitz an”