Hf­-Nd-­Pb isotope evidence from Permian arc rocks for the long-term presence of the Indian-Pacific mantle boundary in the SW Pacific

O. Nebel, C. Münker, Y.J. Nebel-Jacobsen, T. Kleine, K Mezger, N. Mortimer

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    Trace element and initial Hf-Nd-Pb isotopic composition of a series of late Paleozoic arc rocks from South Island, New Zealand show evidence for the presence of Indian-type mantle in the Permian SW Pacific. The trace element budget points to a fluid-dominated arc setting such that Pb isotope compositions for both the volcanic and intrusive rocks were controlled by addition of fluids derived from the subducted slab to the mantle wedge. Relatively unradiogenic initial
    Original languageEnglish
    Pages (from-to)377-392
    JournalEarth and Planetary Science Letters
    Volume245
    DOIs
    Publication statusPublished - 2007

    Fingerprint

    Dive into the research topics of 'Hf­-Nd-­Pb isotope evidence from Permian arc rocks for the long-term presence of the Indian-Pacific mantle boundary in the SW Pacific'. Together they form a unique fingerprint.

    Cite this