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OROGENIC HIGH-PRESSURE PERIDOTITES OF KAN TERRANE - POSSIBLE SOURCE OF DIAMONDS FOR ALLUVIUM OF THE SOUTH PART OF THE SIBERIAN PLATFORM (RUSSIA)

OROGENIC HIGH-PRESSURE PERIDOTITES OF KAN TERRANE - POSSIBLE SOURCE OF DIAMONDS FOR ALLUVIUM OF THE SOUTH PART OF THE SIBERIAN PLATFORM (RUSSIA)

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TSYPUKOV, MIKHAIL
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