182W and 187Os constraints on the origin of siderophile isotopic heterogeneity in the mantle-Reference-Cited by-同舟云学术

182W and 187Os constraints on the origin of siderophile isotopic heterogeneity in the mantle

Published:2023-12 Issue: Volume:363 Page:15-39
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Walker Richard J.^ORCID,Mundl-Petermeier Andrea,Puchtel Igor S.^ORCID,Nicklas Robert W.^ORCID,Hellmann Jan L.,Echeverría Lina M.,Ludwig Kyle D.^ORCID,Bermingham Katherine R.^ORCID,Gazel Esteban,Devitre Charlotte L.,Jackson Matthew G.,Chauvel Catherine^ORCID

Funder

ERC

Engineering Research Centers

Austrian Science Fund

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

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5. 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. Journ. Mass Spectrom.,2017

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1. Evolution of tungsten isotope systematics in the Mauna Kea volcano provides new constraints on anomalous µ182W and high 3He/4He in the mantle;Earth and Planetary Science Letters;2024-08

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