Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; May-June 2007; v. 92; no. 5-6; p. 799-810; DOI: 10.2138/am.2007.2281
© 2007 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Ketcham, R. A.
Right arrow Articles by Hurford, A. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Improved modeling of fission-track annealing in apatite

Richard A. Ketcham1,*, Andrew Carter2, Raymond A. Donelick3, Jocelyn Barbarand4 and Anthony J. Hurford2

1 Jackson School of Geosciences, University of Texas, Austin, Texas, U.S.A.
2 Research School of Earth Sciences at University College of London, U.K.
3 Apatite to Zircon, Inc., Viola, Idaho, U.S.A.
4 Département des Sciences de la Terre, Université Paris Sud, Orsay-Cedex, France

Correspondence: * E-mail: ketcham{at}mail.utexas.edu

Two abiding issues impact the reliability of apatite fission-track analysis and thermal history inversion in particular: reproducibility of track-length measurements and variability of annealing kinetics. In the companion to this paper, we addressed the first by demonstrating that using c-axis projection to normalize track lengths for crystallographic angle improves reproducibility among measurements acquired by Barbarand et al. (2003a, 2003b). We continue here by looking at the effect of c-axis projection on extrapolation of laboratory measurements to geological time scales. We find that c-axis projection improves agreement between predictions of empirical annealing models fit to measurements by Barbarand et al. (2003b) analysts 1 and 3, further corroborating its effectiveness in ameliorating observer bias. Furthermore, these annealing models closely match predictions from the Carlson et al. (1999) annealing data set, which was obtained by a different analyst using a different etching protocol. Normalizing for angle thus allows us to create a single annealing model that encompasses both data sets and etching techniques. By combining the different compositional varieties of apatite in the two data sets, the resulting model provides an improved basis for estimating apatite kinetic properties in unknowns using proxies such as composition, etch-figure dimension, and unit-cell parameters. Predictions from a fanning curvilinear model form accord with conventional expectations of annealing at high and low temperatures, and its use for thermal history inversion will not introduce spurious late cooling events.

Key Words: Fission-track • apatite • annealing • anisotropy • thermochronology • fanning point




This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
C. Glotzbach, C. Spiegel, J. Reinecker, M. Rahn, and W. Frisch
What perturbs isotherms? An assessment using fission-track thermochronology and thermal modelling along the Gotthard transect, Central Alps
Geological Society, London, Special Publications, January 1, 2009; 324(1): 111 - 124.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America