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- W2088317659 abstract "Noble gas studies of oceanic basalts show the ubiquitous presence of an air-like component, which is usually attributed to a simple atmospheric contamination. However, simultaneous nitrogen and argon isotopic study shows the presence of heavy nitrogen with an isotopic composition (δ15N) ∼ +18‰, accompanied by 40Ar/36Ar values much lower than the mantle value. Such a component can be attributed to recycled materials from subduction zones, which are incorporated into these basaltic magmas during their ascent through a shallow enriched region in the mantle. This suggests that a part of the air-like noble gases in oceanic basalts is due to recycled atmospheric gases. Thus the air-like noble gases in the oceanic basalts, hitherto considered a hindrance, provide useful clues for understanding the geochemical evolution of these samples." @default.
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- W2088317659 date "2000-06-01" @default.
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- W2088317659 title "Origin of air-like noble gases in oceanic basalts" @default.
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- W2088317659 doi "https://doi.org/10.1029/1999gl008465" @default.
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