Mathematics
Logic
Scientist
Lamont-Doherty Geological Observatory, Palisades, NY
Lamont-Doherty Earth Observatory of Columbia Univ., Palisades, NY, US
Lamont-Doherty Geological Observatory and Department of Geological Sciences, Columbia University, Palisades, NY 10964 USA
Center for Geoalchemy, Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
Lamont-Doherty Geological Observatory, Department of Geological Sciences, Columbia University, Palisades, NY 10964 USA
Lamont-Doherty Geological Observatory of Columbia University Palisades, NY 10964, USA
Lamont-Doherty Earth Observatory, Palisades, NY
Columbia University, Palisades, NY, US
Lamont-Doherty Geological Observatory; Columbia University, Palisades, NY
Lamont-Doherty Geological Observatory, Palisades, NY 10964 USA
Lamont-Doherty Geological Observatory; Columbia Univ., Palisades, NY
Columbia Univ., Palisades, NY, US
Lamont-Doherty Geological Observatory, Columbia University, Palisades, NY 10964 USA
Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA
Lamont-Doherth Earth Observatory of Columbia University, 10964, Palisades, NY, USA
Lamont-Doherty Geological Observatory of Columbia University, Palisades, NY 10964, and Department of Geological Sciences, Columbia University, New York, NY 10027 USA
Lamont-Doherty Geological Observatory of Columbia University, Palisades, NY 10964, USA
234U/238U mass spectrometry of corals: How accurate is the U-Th age of the last interglacial period?
A major and trace element and strontium, neodymium, and osmium isotopic study of a thick pyroxenite layer from the Beni Bousera Ultramafic Complex of northern Morocco
An isotopic study of the Ni-Cu-PGE-rich Wellgreen intrusion of the Wrangellia Terrane: Evidence for hydrothermal mobilization of rhenium and osmium
Calibration of the C-14 timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals
Constraints on the degree of dynamic partial melting and source composition using concentration ratios in magmas
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