Physics
Scientist
Geol. and Env. Sciences, Stanford Univ., Stanford, CA 94305, USA
Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
Geol. and Env. Sciences, Stanford University, Stanford, CA 94305, USA
Dartmouth College, Hanover, NH
Department of Environmental Earth System Sciences, Stanford University, Stanford, California 94305-2115, USA
Lehigh Univ., Bethlehem, PA, US
Department of Earth Sciences, Dartmouth College, Hanover, NH, USA
Department of Earth Sciences, Dartmouth College, Hanover, USA
Environmental Earth System Science, Stanford University, Stanford, CA 94305, USA
Stanford University, Department of Geological and Environmental Sciences, Stanford, CA 94305, USA
Department of Geological and Environmental Sciences, Stanford University, Stanford, CA, USA
Geological and Environmental Sciences, 320 Lomita Mall, Stanford University, Stanford, CA 94305, USA
Earth and Environmental Systems Science, Stanford University, Stanford, CA 94305, USA
Department of Geological and Environmental Sciences, Stanford University, Building 320, Lomita Mall, Stanford, CA 94305, USA
Department of Geological and Environmental Sciencs, Stanford University, Stanford, California 94305 USA
Department of Environmental Earth System Science, Stanford University, 450 Serra Mall, Braun Hall, Building 320 Stanford University, Stanford, CA 94305, USA
Department of Earth Sciences, Dartmouth College, Hanover, NH 03755, USA
Wien Univ., Austria.
Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115, USA
Department of Earth Sciences, Dartmouth College, Hanover, NH 03755 USA
Geological and Environmental Sciences, 320 Lomita Mall, Stanford University, California 94305, USA
Department of Environmental Earth System Science, Stanford University, Stanford, CA 94305, USA
Departm
A Late Miocene stable isotope paleosoil record of Andean foreland precipitation
Are high 3He/4He ratios in oceanic basalts an indicator of deep-mantle plume components?
Boiling fluids in a region of rapid uplift, Nanga Parbat Massif, Pakistan
Ca/Sr and Sr isotope systematics of a Himalayan glacial chronosequence: carbonate versus silicate weathering rates as a function of landscape surface age
Cenozoic topographic and climatic response to changing tectonic boundary conditions in Western North America
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