Concentration of radioactive elements in deep crustal material

Mathematics – Logic

Scientific paper

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Scientific paper

Th, U and K have been determinedin paragneisses of different metamorphic grade. Both Th and U concentrations are lower in granulite facies rocks than in more low-grade metamorphic rocks of equivalent nature. Thus geological processes operating in the crust must result in an upward concentration of these elements. The Th / U ratio of the paragneisses shows a wide variation which is related to the oxidation of U. Some evidence exists for a decrease of the Th / U ratios with metamorphic grade.

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