Abstract
An assemblage of chernovite-(Y), As-bearing thorite, rooseveltite, and Cu and Fe arsenates has been revealed in Li-F granites, ongonites, and greisens of the Far East. The formation sequence of the above minerals is described in this paper. Chernovite-(Y) is a product of autometasomatic alteration of Li-F granite and ongonite, whereas other arsenates and As-thorite are products of greisenization.
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