Bulk silicate Earth-like 142Nd and 182W mantle component sampled by 2.0 Ga Onega Basin picrites, Fennoscandia

IS Puchtel, JL Hellmann, H Rizo, J Blichert-Toft… - … et Cosmochimica Acta, 2025 - Elsevier
In order to further evaluate the timing and possible mechanisms responsible for the
transition from both positive and negative to no 142 Nd and 182 W anomalies in the Archean …

A Systematic Investigation of the Effects of Standard‐Sample Concentration Mismatch during Fe Isotope Measurement by MC‐ICP‐MS

EK King‐Doonan, LD Bilenker, D Weis… - Geostandards and …, 2024 - Wiley Online Library
Advances in multi‐collector inductively coupled plasma‐mass spectrometry (MC‐ICP‐MS)
have led to the widespread use of iron (Fe) isotopes to elucidate the (bio) geochemical …

Iron isotope heterogeneity in magmas of subduction zones and its origin

R Liao, H Zhu, C Li, H Liu, W Sun - Lithos, 2023 - Elsevier
Iron isotope heterogeneity of subduction-related primitive magmas was traditionally thought
to be predominantly attributed to the addition of slab-derived components. However, the …