Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6434196 | Tectonophysics | 2012 | 7 Pages |
Luminescence technique has been shown to have great potential in low-temperature (< 100 °C) themochronology. This study investigates the kinetic process of luminescence in a cooling system. We present a new formula that can be used for determining the cooling age based on luminescence-thermochronology. The cooling rate can be obtained directly from a plot of luminescence age versus the present temperature. We show that the application and capacity of luminescence-thermochronology are significantly controlled by the saturation of luminescence and environmental dose rate.
⺠We present new formulas and methods to be used in luminescence thermochronology. ⺠The cooling rate can be obtained directly from a plot of luminescence age versus temperature. ⺠The concept of closure temperature cannot be simply applied to luminescence thermochronology. ⺠Potentials of luminescence thermochronology are discussed.