Title
Further investigation of the initial fission-track length and geometry factor in apatite fission-track thermochronology
Date Issued
01 January 2013
Access level
metadata only access
Resource Type
journal article
Author(s)
Soares C.J.
Guedes S.
Lixandrão Filho A.L.
Osório A.M.
Alencar I.
Dias A.N.C.
Hadler J.
Universidad Estatal Paulista
Publisher(s)
Walter de Gruyter GmbH
Abstract
The external detector method (EDM) is a widely used technique in fission track thermochronology (FTT) in which two different minerals are concomitantly employed: spontaneous tracks are observed in apatite and induced ones in the muscovite external detector. They show intrinsic differences in detection and etching properties that should be taken into account. In this work, new geometry factor values, g, in apatite, were obtained by directly measuring the ρed/ρis ratios and independently determined [GQR]ed/is values through the measurement of projected lengths. Five mounts, two of which were large area prismatic sections and three samples composed of random-orientation pieces have been used to determine the g-values. A side effect of applying EDM is that the value of the initial confined induced fission track, L0, is not measured in routine analyses. The L 0-value is an important parameter to quantify with good confidence the degree of annealing of the spontaneous fission tracks in unknown-age samples, and is essential for accurate thermal history modeling. The impact of using arbitrary L0-values on the inference of sample thermal history is investigated and discussed. The measurement of the L0-value for each sample to be dated using an extra irradiated apatite mount is proposed. This extra mount can be also used for determining the g value as an extension of the ρed/ρis ratio method. Eight apatite samples from crystalline basement, with grains at random orientation, were used to determine the g-values. The results found are statistically in agreement with the values found for apatite samples (from Durango, Mexico) measured in prismatic section and also measured at random orientation. There was no observable variation in efficiency regarding crystal orientation, showing that it is relatively safe using non-prismatic grains, especially in samples with paucity of grains, as it is the case of most basin samples. Implications for the ζ-calibration and for the calibration of the direct (spectrometer-based) fission-track dating are also discussed.
Start page
1381
End page
1392
Volume
98
Issue
September 8
Language
English
OCDE Knowledge area
Geociencias, Multidisciplinar
Scopus EID
2-s2.0-84882771211
Source
American Mineralogist
ISSN of the container
0003004X
Sponsor(s)
We thank Richard Ketcham and Jocelyn Barbarand for their constructive comments that helped improve the manuscript. This work is part of C.J. Soares’s Ph.D. research and was financially supported by Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP, Brazil) and Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq, Brazil).
Sources of information: Directorio de Producción Científica Scopus