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36Cl (T1/2=3.01× 105 a) is one of the most widely studied radioactive nuclides. It can be produced both in the atmosphere and lithosphere by a variety of nuclear reactions. In the case of 36Cl in limestone, the most important reactions are the following:
36Cl (T1 / 2 = 3.01 × 105 a) is one of the most widely studied radioactive nuclides. It can be produced both in the atmosphere and lithosphere by a variety of nuclear reactions. In the case of 36Cl in limestone, the most important reactions are the following: