Mathematics – Logic
Scientist
Mathematics
Logic
Scientist
Northwestern University, Evanston, IL
Washington University, St. Louis, MO
Washington University in St. Louis, Department of Earth and Planetary Sciences, 1 Brookings Drive, St. Louis, MO 63130, USA
Department of Earth and Planetary Sciences, One Brookings Dr., Campus Box 1169, Washington University, St. Louis, MO, 63230, USA
Department of Earth and Planetary Sciences, Washington University in St. Louis, 1 Brookings Drive, St. Louis, MO 63130, USA of Earth and Planetary Sciences, Washington University, Saint Louis, Missouri 63130 USA
Department of Earth and Planetary Sciences, Washington University, St Louis, MO 63130, USA
Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri, USA
Department of Earth and Planetary Sciences, Washington University, St. Louis, MO, USA
Department of Earth and Planetary Sciences, Washington University, St. Louis, MO, 63130, USA Washington University, Campus Box 1169, One Brookings Dr St. Louis, MO, 63130, USA
Department of Geological Sciences, Northwestern University, Evanston, IL 60201 USA
Department of Earth and Planetary Sciences, Washington University, 1 Brookings Dr., 63130, St. Louis, MO, USA
Washington University, Saint Louis, MO
Department of Earth and Planetary Sciences, Washington University in St. Louis, MO, USA
Department of Earth and Planetary Sciences, Washington University, 1 Brookings Drive, St. Louis, MO 63130, USA
Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA
Department of Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, MO 63130, USA
A diffuse plate boundary model for Indian Ocean tectonics
A further proposal for additional regions for the Flinn?Engdahl Regionalization Scheme
A teleseismic shear-wave splitting study to investigate mantle flow around South America and implications for plate-driving forces
Aftershock locations and rupture characteristics of the 1995 Mariana deep earthquake
Aftershock sequences of moderate-sized intermediate and deep earthquakes in the Tonga subduction zone
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