Lateral Zonality of the East Sikhote-Alin Volcanic Belt: Geodynamic Regime in the Late Cretaceous
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DOI: 10.1134/s1819714019030060
Abstract: The East Sikhote Alin volcanic belt (~1500 km long) is commonly regarded as a tectonomagmatic structure formed in the Late Cretaceous in a subduction environment, which was followed by the destruction of the oceanic slab… read more here.
Keywords: late cretaceous; sikhote alin; belt; east sikhote ... See more keywords