Calc-alkaline magmatism of the Omgon Range: Evidence for Early Paleogene extension in the Western Kamchatka segment of the Eurasian continental margin.

Calc-alkaline magmatism of the Omgon Range: Evidence for Early Paleogene extension in the Western Kamchatka segment of the Eurasian continental margin.

Ledneva, G V; Nosova, A A; Soloviev, A V
xmlui.dri2xhtml.METS-1.0.item-citation: Ledneva, G V; Nosova, A A; Soloviev, A V (2006): Calc-alkaline magmatism of the Omgon Range: Evidence for Early Paleogene extension in the Western Kamchatka segment of the Eurasian continental margin. Petrology, 14(2), 154-186, https://doi.org/10.1134/S0869591106020020
Date: 2006-08-13

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