Eiler, John M. and Valley, John W. and Baumgartner, Lukas P. (1992) Oxygen isotope diffusion: applications to thermometry and fluid flow. Abstracts with Programs - Geological Society of America, 24 (7). A250. ISSN 0016-7592. https://resolver.caltech.edu/CaltechAUTHORS:20130710-133604311
Full text is not posted in this repository.
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20130710-133604311
Abstract
Interdiffusion of stable isotopes will strongly influence the fractionations and intracrystalline zonation of slowly cooled igneous and metamorphic rocks. Previous attempts to quantify the effects of stable isotope interdiffusion during cooling (Dodson, 1973; Javoy, 1977; Giletti, 1986) have revealed its importance, but were based on an inaccurate description of the interdiffusion process. The Fast Grain Boundary (FGD) model for interdiffusion (Eiler et al., 1991 GSA; 1992 in press) provides the first model for accurately quantifying the dependence of stable isotope closure temperatures and diffusion profiles on grain size, grain shape, cooling rate, and mineral abundance.
| Item Type: | Article |
|---|---|
| Additional Information: | © 1992 Geological Society of America. |
| Issue or Number: | 7 |
| Record Number: | CaltechAUTHORS:20130710-133604311 |
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20130710-133604311 |
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. |
| ID Code: | 39289 |
| Collection: | CaltechAUTHORS |
| Deposited By: | Tony Diaz |
| Deposited On: | 20 Sep 2013 20:04 |
| Last Modified: | 03 Oct 2019 05:05 |
Repository Staff Only: item control page
