Mathematics
Logic
Scientist
Purdue University, West Lafayette, Ind.
Comparison of trace elements in L3-6 chondrites and artificially heated Krymka (L3)
Contents of eleven trace elements in ureilite achondrites
Radium-thorium disequilibrium and zeolite-water ion exchange in a Yellowstone hydrothermal environment
Thermal metamorphism of primitive meteorites. II - Ten trace elements in Abee enstatite chondrite heated at 400-1000 C
Thermal metamorphism of primitive meteorites. III - Ten trace elements in Krymka L3 chondrite heated at 400-1000 C
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