Evolution of tungsten isotope systematics in the Mauna Kea volcano provides new constraints on anomalous µ182W and high 3He/4He in the mantle
Highly siderophile element abundances and 182 W/184 W and 187 Os/188 Os were
determined for a suite of Mauna Kea lavas from the Hawaiian Scientific Drilling Project …
determined for a suite of Mauna Kea lavas from the Hawaiian Scientific Drilling Project …
W-Fe isotopes argue against OIB-like basalts in Inner Mongolia originating from primordial peridotite mantle
Abstract Whether Inner Mongolia OIB-like basalts originate from the modern upper mantle
[eg depleted MORB mantle (DMM)] with recycled oceanic crust in the form of pyroxenite or …
[eg depleted MORB mantle (DMM)] with recycled oceanic crust in the form of pyroxenite or …
Dynamical Geochemistry: Mantle dynamics and its role in the formation of geochemical heterogeneity
Chemical geodynamics is a term coined nearly forty years ago to highlight the important link
between Earth's geochemical evolution and plate tectonics & mantle convection. Significant …
between Earth's geochemical evolution and plate tectonics & mantle convection. Significant …