Strontium and Neodymium Isotopic Signatures in Basalt Glasses of the Mid-Atlantic Ridge, 12°–31° N
Author:
Publisher
Pleiades Publishing Ltd
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1134/S0016702923120054.pdf
Reference43 articles.
1. N. S. Bortnikov, S. A. Silantev, F. Bea, P. Montero, T. F. Zinger, S. G. Skolotnev, and E. V. Sharkov, “Multiple melting of a heterogeneous mantle and episodic accretion of oceanic crust in a spreading zone: zircon U-Pb Age and Hf-O Isotope Evidence from an Oceanic Core Complex of the Mid-Atlantic Ridge,” Petrology 30 (1), 1–24 (2022).
2. H. Bougault, L. Dmitriev, J. G. Schilling, A. Sobolev, J. L. Joron, and H. D. Needham, “Mantle heterogeneity from trace elements: MAR triple junction near 14° N,” Earth Planet. Sci. Lett. 88, 27–36 (1988).
3. A. I. Buikin, S. A. Silantyev, and A. B. Verchovsky, “N‒Ar–He–CO2 systematics combined with H2O, Cl, K abundances in MORB glasses demonstrate interaction of magmatic and hydrothermal systems: a case for MAR at 16°07′–17°11′ N,” Geochem. Int. 60 (11), 1068–1086 (2022).
4. D. J. DePaolo, “Crustal growth and mantle evolution: inferences from models of element transport and Nd and Sr isotopes,” Geochim. Cosmochim. Acta 44, 1185–1196 (1980).
5. D. J. DePaolo, “The mean life of continents: estimates of continental recycling rates from Nd and Hf isotopic data and implications for mantle structure,” Geophys. Res. Lett. 10, 705–708 (1983).
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