Abstract

Luminescence signals from quartz and feldspar contain a wealth of information about exposure to heat and sunlight. While many studies have focused on quantifying individual processes such as grain transport and burial, cooling during exhumation, or bleaching of freshly exposed rock surfaces, not much work has yet been done to illustrate how these effects might interact. For example, how might a geomorphologist interpret the luminescence signals within a riverine cobble or within a recent rockfall from an uplifting terrain? This study attempts to address this issue by first presenting a simple kinetic expression for OSL signal accumulation in response to background radiation, and OSL loss by exposure to heat or to direct or attenuated sunlight. This model is then used to simulate three example sample histories. Simulation results demonstrate how much information can be embedded within one sample's luminescence signal and how disparate geomorphic histories can produce strikingly similar signals. The temperatures and timescales which can be examined with luminescence signals are presented in comparison to those of various geomorphic processes. Finally, simulation results illustrate the benefit of using signals of different stability to better understand a sample's recent geologic history.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.