Using of 53Mn and 10Be Cosmogenic Isotopes for Geochronology and Monitoring of Cosmic Rays in Terrestrial Rocks
Volume 1, Issue 1, December 2016, Pages: 24-28
Received: Dec. 2, 2016;
Accepted: Dec. 26, 2016;
Published: Jan. 19, 2017
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V. E. Yants, Institute for Nuclear Research of Russian Academy of Sciences, Department of Experimental Physics, 60th October Anniversary Prospect, Moscow, Russian Federation
S. G. Lebedev, Institute for Nuclear Research of Russian Academy of Sciences, Department of Experimental Physics, 60th October Anniversary Prospect, Moscow, Russian Federation
N. M. Sobolevsky, Institute for Nuclear Research of Russian Academy of Sciences, Department of Experimental Physics, 60th October Anniversary Prospect, Moscow, Russian Federation
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The article discusses the methods of measuring the accumulation of radioactive isotopes 53Mn (with a half-life of T = 3.7 million years) and 10Be (T = 1.6 million years) in the iron-containing rocks. Knowledge of accumulation dynamics of these two isotopes would allow knowing both the time of shielding and flux of cosmic rays and also changes assessing the variations in the intensity of cosmic rays, the timing of glaciations, geological changes, and climatic processes in the world in retrospect of 0.1-10 million years. The main attendance paying to neutron - activation method of isotope analysis as low-cost both in money and time and more adapted for numerous sample processing. The advantages of isotope measurements in lunar craters are emphasized.
Cosmic Rays, Cosmic Rays Variations, Radioactive Isotopes, Isotopes Accumulation, Geological Changes
To cite this article
V. E. Yants,
S. G. Lebedev,
N. M. Sobolevsky,
Using of 53Mn and 10Be Cosmogenic Isotopes for Geochronology and Monitoring of Cosmic Rays in Terrestrial Rocks, Nuclear Science.
Vol. 1, No. 1,
2016, pp. 24-28.
Copyright © 2016 Authors retain the copyright of this article.
This article is an open access article distributed under the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/
) which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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