Variation of thorium and uranium in selected granitic rocks

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Scientific paper

A selected suite of granitic rocks representing both individual differentiation sequences and a broad sampling of granites from North America have been analysed for thorium, uranium, and potassium by -ray spectrometry. In the White Mountain and Oliverian series of New Hampshire both the thorium and uranium contents and the Th/U ratio tend to increase with igneous evolution. In the Southern California batholith the thorium and uranium contents increase during differentiation, but the Th/U ratio is constant. The general tendency for the Th/U ratio to increase with petrogenetic evolution is shown by a comparison of the Th/U ratio with the ratio of potassium feldspar to plagioclase for a broad sampling of granitic rocks. This increase is probably caused by oxidation during magmatic differentiation

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