Abstract
It is shown that the giant Sikhote-Alin and Pamir deposits of boron are associated with fragments of the boron-bearing evaporite strata of paleoceanic atolls in the subduction melange. Ore formation relates both to in situ transformation of boron-bearing evaporite strata at the Ak-Arkhar deposit and to boron mobilization and redeposition some distance away from the evaporite source in course of intensive post-accretionary fluid-magmatic reworking of the subduction melange at the Dalnegorskoe deposit.
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