Electron spin resonance dating
The conference invites contributions from this broad range of applications, including Quaternary geology, geomorphology and landscape evolution, palaeontology, palaeobotany, archaeology, soil science, palaeoclimatology, provenancing, mineral prospecting, tectonics, space science, dose-rate assessment, retrospective population dosimetry and radiological event studies, including relating to the aftermath of the 2011 Tohoku earthquake.
Contributions are also invited on applications to new materials, current developments and methodological aspects of ESR, Thermoluminescence and Radioluminescence, and novel Optical Dating techniques such as TT-OSL and PIR-IRSL.
The total radiation dose which the crystals have received during their geologic history is determined from the natural ESR signal and the signal growth curves after artificial irradiation.
Counting measurements of the radioactive impurity content of the sample were used to compute the annual natural radiation dose.
Including non-dating applications of luminescence and ESR (APLED-4) Nov 22nd, 2015, Dosi Vox Workshop (optional)Nov 23rd-25th, 2015, Conference, Adelaide, Australia Nov 26-28th, 2015, Field Trip, Naracoorte, South Australia The Braggs Building School of Physical Sciences & Institute for Photonics and Advanced Sensing University of Adelaide, Adelaide, South Australia, 5005, Australia The conference seeks to bring together researchers to present new developments in Luminescence and ESR, with particular focus on techniques, applications and issues relevant to the Asia-Pacific region.
Voinchet P, Despriée J, Tissoux H, Falguères C, Bahain JJ, Gageonnet R, Dépont J & Dolo JM (2010) ESR chronology of alluvial deposits and first human settlements of the Middle Loire Basin (Region Centre, France).
A new method of geologic age determination using electron spin resonance to measure trapped charge in minerals has been developed and tested.
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