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Lopend onderzoek (11)
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(het meest recente onderzoek is bovenaan geplaatst)
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What controls the distribution of trace elements during partial melting of silicates in planetary interiors?
Penvoerder
Exploring the Earth's earliest oceans with silicon: magnitudes of isotopic fractionation
Penvoerder
Petrology
Penvoerder
Terminal stage collision magmatism along the western Tethys suture
Penvoerder
Unraveling the key controls of bauxite formation in Suriname
Penvoerder
Terrestrial volcanic lakes as analogues for Martian sulfate rich terrains
Penvoerder
Testing the robustness of the sulfur stable isotope biomarker and paleoredox indicator for planetary exploration
Penvoerder
Tracing Early Planetary Life using combined Fe and S stable isotopes
Penvoerder
The role of perchlorates in the preservation of organic compounds on Mars
Penvoerder
Tracing novel selenium metabolisms in the geological record using selenium stable isotopes
Penvoerder
Reactive Oxygen Species on the early Earth: Exobiological Implications
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