US Geological Survey
Date of this Version
2010
Citation
Quaternary Geochronology 6 (2011) 61-70
doi:10.1016/j.quageo.2010.04.002
Abstract
The possibility of dating basalt using luminescence was tested on four samples with independent age control from Cima volcanic !eld, California, with the ultimate aim of assessing whether the technique could be used to date sediments on the surface of Mars. Previous analysis of these samples had demonstrated that the infrared stimulated luminescence (IRSL) signal is most suitable for dating as it showed the lowest fading rate among various luminescence signals. In this study, changes in equivalent dose as a function of preheat are described. The ages for the two youngest Cima samples agree with the independent ages based on cosmogenic nuclide measurements (12.0 ! 0.8 ka). In the two older samples (dated to 320 and 580 ka by KeAr), the luminescence behaviour is more complex and the form of the IRSL decay curve is seen to vary with dose. Mathematical !tting is used to isolate two components and their intensities are used to produce dose response curves. The slower component yields a larger equivalent dose. However, even using this component and after correction for fading, the ages obtained for the older samples are younger than the KeAr ages.
Included in
Geology Commons, Oceanography and Atmospheric Sciences and Meteorology Commons, Other Earth Sciences Commons, Other Environmental Sciences Commons
Comments
U.S. government work