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The Permian-Triassic Boundary in the Eastern Part of the USSR
The Upper Permian and Lower Triassic marine sediments of the Upper Kolyma region in Verkhoyanie, the Omolon massif, Transbaikalie, central Priamurie and southern Primorie are briefly described. The Permian-Triassic boundary is usually paraconformable, locally conformable and prominently disconformable only in the southern Primorie.
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