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carbonated mantle source

This result, together with the low-SiO2 contents, relative depletion of Zr–Hf–Ti, and high δ 66 Zn characteristics of these strongly alkaline rocks, suggests derivation from a carbonated mantle source.

Molybdenum and boron isotope evidence for fluid-fluxed melting of intraplate upper mantle beneath the eastern North China Craton

carbonated mantle source

Low‐δMg basalts are commonly interpreted to represent melts derived from carbonated mantle sources.

Light Mg Isotopic Composition in the Mantle Beyond the Big Mantle Wedge Beneath eastern Asia

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10.1016/J.EPSL.2019.05.038

This result, together with the low-SiO2 contents, relative depletion of Zr–Hf–Ti, and high δ 66 Zn characteristics of these strongly alkaline rocks, suggests derivation from a carbonated mantle source.

Molybdenum and boron isotope evidence for fluid-fluxed melting of intraplate upper mantle beneath the eastern North China Craton

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10.1029/2018JB016857

Low‐δMg basalts are commonly interpreted to represent melts derived from carbonated mantle sources.

Light Mg Isotopic Composition in the Mantle Beyond the Big Mantle Wedge Beneath eastern Asia

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10.1016/J.LITHOS.2019.02.006

Plio-Quaternary Golcuk potassic magmas were possibly derived from partial melting of carbonated mantle metasomes under an extensional tectonic regime.

40Ar-39Ar dating and petrology of monzonite ejecta in tephra from Quaternary Gölcük volcano (Isparta, SW Turkey): tear-related contrasting metasomatic symptoms in extensional mantle-derived magmas

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Carbonated Mantle - This result, together with the low-SiO2 contents, relative depletion of Zr–Hf–Ti, and high δ 66 Zn characteristics of these strongly alkaline rocks, suggests derivation from a carbonated mantle source. [1] Low‐δMg basalts are commonly interpreted to represent melts derived from carbonated mantle sources. [2] Plio-Quaternary Golcuk potassic magmas were possibly derived from partial melting of carbonated mantle metasomes under an extensional tectonic regime. [3]

carbonated mantle source

This result, together with the low-SiO2 contents, relative depletion of Zr–Hf–Ti, and high δ 66 Zn characteristics of these strongly alkaline rocks, suggests derivation from a carbonated mantle source. [1] Low‐δMg basalts are commonly interpreted to represent melts derived from carbonated mantle sources. [2]