Evolution of tungsten isotope systematics in the Mauna Kea volcano provides new constraints on anomalous µ182W and high 3He/4He in the mantle-Reference-Cited by-同舟云学术

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Evolution of tungsten isotope systematics in the Mauna Kea volcano provides new constraints on anomalous µ182W and high 3He/4He in the mantle

Published:2024-08 Issue: Volume:640 Page:118795
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Willhite Lori N^ORCID,Finlayson Valerie A^ORCID,Walker Richard J^ORCID

Publisher

Elsevier BV

Reference69 articles.

1. Lead isotopes reveal bilateral asymmetry and vertical continuity in the Hawaiian mantle plume;Abouchami;Nature,2005

2. Origin of 182W anomalies in ocean island basalts;Archer;Geochem., Geophys., Geosyst.,2023

3. High-precision analysis of 182W/184W and 183W/184W by negative thermal ionization mass spectrometry: per-integration oxide corrections using measured 18O/16O;Archer;Int. J. Mass Spectrom.,2017

4. Chemical variations and regional diversity observed in MORB;Arevalo;Chem. Geol.,2010

5. Tungsten geochemistry and implications for understanding the Earth's interior;Arevalo;Earth Planet. Sci. Lett.,2008

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