Concentration changes of thorium, uranium and other metals in hydrothermally altered Conway granite, New Hampshire

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Scientific paper

Concentrations of Th, U, K, Mg, Ca, Mn, Fe, Zn, Co and Cu are
significantly different in two sections of a 1000 foot core sample of
Conway granite. The differences, attributable to the action of weak
hydrothermal fluids, indicate that the fluids, though weak, caused
effective redistribution of these elements.

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