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Hledat publikace relevantní k dotazu "Sodalite olivine-poor nephelinite (age 25.6 Ma) differs from similar rocks of Cenozoic province - enrichment in REE. 87Sr/86Sr and 143Nd/144Nd ratios are consistent with HIMU OIB from sublithospheric depleted mantle source."
Sodalite olivine-poor nephelinite (age 25.6 Ma) differs from similar rocks of Cenozoic province - enrichment in REE. 87Sr/86Sr and 143Nd/144Nd ratios are consistent with HIMU OIB from sublithospheric depleted mantle source.
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Geochemically anomalous olivine-poor nephelinite of Říp Hill, Czech Republic
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