Physics
Scientist
Anoxic dissolution processes of biotite: implications for Fe behavior during Archean weathering
Atmospheric oxygen rise in the Paleoproterozoic revealed by weathering model
Fe isotope compositions of 1.85 Ga Flin Flon paleosol, Canada
Kinetics of biotite dissolution and Fe behavior under low O2 conditions and their implications for Precambrian weathering
O2 evolution in the Paleoproterozoic: Experimental simulation of the relationships between Fe in paleosols and PO2
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