Anomalously nucleogenic neon in North Chile Ridge basalt glasses suggesting a previously degassed mantle source

Details Anomalously nucleogenic neon in North Chile Ridge basalt glasses suggesting a previously degassed mantle source Anomalously nucleogenic neon in North Chile Ridge basalt glasses suggesting a previously degassed mantle source

Aug 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998e%26psl.160..447n&link_type=abstract

Earth and Planetary Science Letters, vol. 160, Issue 3-4, pp.447-462

Computer Science

7

Chile Ridge, Mid-Ocean Ridge Basalts, Neon, Noble Gases

Scientific paper

Fresh basalt glasses from the North Chile Ridge (NCR) in the southeastern Pacific have Ne isotopic compositions distinctly different from typical mid-ocean ridge basalts (MORB). In a three-isotope plot of 20 Ne/ 22 Ne vs. 21 Ne/ 22 Ne, the NCR data define a correlation line with a slope smaller than that of the MORB correlation line, i.e. their Ne composition is more nucleogenic than that of MORB. 3 He/ 4 He ratios are slightly lower than the MORB average, whereas in a few stepwise heating fractions very high 40 Ar/ 36 Ar ratios up to 28,000 are found. One model to explain the data assumes contamination of the NCR mantle source by material from the continental or oceanic crust, but in addition to difficulties with quantitatively reconciling the noble gas patterns with such a model it seems unable to account for some geochemical characteristics of NCR basalts reported earlier [Bach et al., Earth Planet. Sci. Lett. 142 (1996) 223-240], such as depletions in highly incompatible elements and unradiogenic Sr isotope compositions. Therefore we favor the scenario of a mantle source which was depleted and degassed previously, possibly as a residue from mantle melting beneath the southern East Pacific Rise that was transported to the NCR and melted again. The time during which such a depleted reservoir would have to be separated from the MORB mantle is estimated at ~10-100 Ma based on U/Th-Ne systematics, in reasonable agreement with the time scale deduced from the formation history of the NCR and the temporal evolution of the southeast Pacific.

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