Mantle transition zone-derived EM1 component beneath NE China: Geochemical evidence from Cenozoic potassic basalts
Abstract
null null The isotopic characteristics of the sub-oceanic mantle are well established, but in continental regions these properties are usually obscured, and therefore controversial, because of the potential effects of crustal contamination together with lithospheric mantle metasomatism and melting. The so-called EM1 (Enriched Mantle-1) signature, characterized by low 206Pb/204Pb and 143Nd/144Nd ratios, is particularly problematic in this respect...
Paper Details
Title
Mantle transition zone-derived EM1 component beneath NE China: Geochemical evidence from Cenozoic potassic basalts
Published Date
May 1, 2017
Volume
465
Pages
16 - 28
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