Geochronology/Thermoluminescences
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
- 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
- ↑ 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.