
handle: 2158/957546
The mantle melting mechanism in two within-plate geodynamic setting (Sicily Channel and Canary Islands) is instigate through U-series disequilibria, Sr-Nd-Pb isotopes and trace elements.
U-series disequilibria; Sr-Nd-Pb isotope; Sicily channel; Canary islands; Within-plate magmatism; Magmatism and geodynamics; Mantle melting
U-series disequilibria; Sr-Nd-Pb isotope; Sicily channel; Canary islands; Within-plate magmatism; Magmatism and geodynamics; Mantle melting
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