Jon Wade

Determining the composition of the Earth

Nucleic Acid Extraction and Sequencing from Low-Biomass Synthetic Mars Analog Soils for In Situ Life Detection

The Drive to Life on Wet and Icy Worlds

Biological safety in the context of backward planetary protection and Mars Sample Return: conclusions from the Sterilization Working Group

Composition of the depleted mantle

Implications of Nb/U, Th/U and Sm/Nd in plume magmas for the relationship between continental and oceanic crust formation and the development of the depleted mantle

Incompatible element ratios in oceanic basalts and komatiites: Tracking deep mantle sources and continental growth rates with time

Development and Geotechnical Engineering Properties of KLS-1 Lunar Simulant

Preparation and Characterization of High-Strength Geopolymer Based on BH-1 Lunar Soil Simulant with Low Alkali Content

Partitioning of Si and O between liquid iron and silicate melt: A two‐phase ab‐initio molecular dynamics study

Hafnium isotopes in Jack Hills zircons and the formation of the Hadean crust

Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust

“New” lunar meteorites: Implications for composition of the global lunar surface, lunar crust, and the bulk Moon

The Lu–Hf and Sm–Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets

Alteration and geochemical patterns in the 3.7–3.8 Ga Isua greenstone belt, West Greenland

Microstructures and properties of high-entropy alloys

The bulk composition of Mars

The Crust of the Moon as Seen by GRAIL

Major and trace element composition of the depleted MORB mantle (DMM)

The Earth's ‘missing’ niobium may be in the core

Accretion of the Earth and segregation of its core

Volcanism on Mars controlled by early oxidation of the upper mantle

The oxidation state and mass of the Moon-forming impactor

Core formation and the oxidation state of the Earth: Additional constraints from Nb, V and Cr partitioning

Core formation and the oxidation state of the Earth