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Bulk silicate Earth-like 142Nd and 182W mantle component sampled by 2.0 Ga Onega Basin picrites, Fennoscandia
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 …
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
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 …
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 …
to be predominantly attributed to the addition of slab-derived components. However, the …