Abstract
No economically attractive quantities of metalliferous ore mineral are found in the extensive sand accumulations between the mouths of the Catlins and Mataura Rivers. A dark green amphibole is the outstandingly predominant heavy mineral throughout. Definite radioactivity is indicated at four places, in three cases in — 60 B.S. mesh “heavy” fractions and in one case in + 44 B.S. mesh unconcentrated material.

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