Melts from hydrous depleted back-arc mantle at a young boninitic volcano on the flank of Valu Fa Ridge (Lau basin, SW Pacific)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-023-02053-5.pdf
Reference100 articles.
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3. Bast R, Scherer EE, Sprung P et al (2015) A rapid and efficient ion-exchange chromatography for Lu–Hf, Sm–Nd, and Rb–Sr geochronology and the routine isotope analysis of sub-ng amounts of Hf by MC-ICP-MS. J Anal at Spectrom 30:2323–2333. https://doi.org/10.1039/C5JA00283D
4. Beier C, Turner SP, Haase KM et al (2017) Trace element and isotope geochemistry of the northern and central Tongan islands with an emphasis on the genesis of high Nb/Ta signatures at the northern volcanoes of Tafahi and Niuatoputapu. J Petrol 58:1073–1106. https://doi.org/10.1093/petrology/egx047
5. Bézos A, Escrig S, Langmuir CH et al (2009) Origins of chemical diversity of back-arc basin basalts: a segment-scale study of the eastern Lau spreading center. J Geophys Res Solid Earth. https://doi.org/10.1029/2008JB005924
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