Article ID Journal Published Year Pages File Type
6434196 Tectonophysics 2012 7 Pages PDF
Abstract

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.

► We present new formulas and methods to be used in luminescence thermochronology. ► The cooling rate can be obtained directly from a plot of luminescence age versus temperature. ► The concept of closure temperature cannot be simply applied to luminescence thermochronology. ► Potentials of luminescence thermochronology are discussed.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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