Anomalous 182W in high 3He/4He ocean island basalts: Fingerprints of Earth’s core?
Abstract
The short-lived 182Hf-182W isotope system (t1/2 = 9 Ma) left evidence in both ancient and modern terrestrial rock record of processes that took place during the earliest stages of Earth’s accretionary and differentiation history. We report µ182W values (the deviation of 182W/184W of a sample from that of laboratory standards, in parts per million) and corresponding 3He/4He ratios for rocks from 15 different hotspots. These rocks are...
Paper Details
Title
Anomalous 182W in high 3He/4He ocean island basalts: Fingerprints of Earth’s core?
Published Date
Feb 1, 2020
Volume
271
Pages
194 - 211
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