Geochronology/Thermoluminescences
Jump to navigation
Jump to search
Thermoluminescence (TL) research was focused on heated pottery and ceramics, burnt flints, baked hearth sediments, oven stones from burnt mounds and other heated objects.[1]
TL can be used to date unheated sediments.[2]
TL dating of light-sensitive traps in geological sediments of both terrestrial and marine origin became more widespread.[3]
See also
[edit | edit source]- Argon–argon dating
- Cathodoluminescence
- Cenozoic
- Chemostratigraphy
- Cosmogenic radionuclide dating
- Dates
- Dendrochronology
- Dye 3
- Electron spin resonance
- Fission track dating
- Geomagnetic Polarity Time Scale
- Ice cores
- Black ice
- Brittle ice
- Clear ice
- Firns
- Sea ice
- Lichenometry
- Magnetostratigraphy
- Marker horizons
- Mesozoic
- Optically stimulated luminescence
- Paleomagnetic dating
- Paleontology
- Paleozoic
- Palynology
- Potassium–argon dating
- Radiocarbon dating
- Stratigraphy
- Tephrochronology
- Thermoluminescence
- Uranium–lead dating
- Uranium-thorium dating
- Varves
References
[edit | edit source]- ↑ Roberts, R.G., Jacobs, Z., Li, B., Jankowski, N.R., Cunningham, A.C., & Rosenfeld, A.B. (2015). "Optical dating in archaeology: thirty years in retrospect and grand challenges for the future". Journal of Archaeological Science 56: 41–60. doi:10.1016/j.jas.2015.02.028. http://www.sciencedirect.com/science/article/pii/S0305440315000667. Retrieved February 16, 2016.
- ↑ Shelkoplyas, V.N.; Morozov, G.V. (1965). "Some results of an investigation of Quaternary deposits by the thermoluminescence method". Materials on the Quaternary Period of the Ukraine 7th International Quaternary Association Congress, Kiev: 83–90.
- ↑ Wintle, A.G. & Huntley, D.J. (1982). "Thermoluminescence dating of sediments". Quaternary Science Reviews 1: 31–53. doi:10.1016/0277-3791(82)90018-X. http://www.sciencedirect.com/science/article/pii/027737918290018X. Retrieved February 16, 2016.