The null hypothesis: steady rates of erosion, weathering and sediment accumulation during Late Cenozoic mountain uplift and glaciation

Jane K. Willenbring, University of Pennsylvania, Department of Earth & Environmental Sciences, Philadelphia, PA, United States and Douglas J Jerolmack, University of Pennsylvania, Department of Earth & Environmental Science, Philadelphia, United States
Back to: Mountain Building, Denudation, and the Global Evolution of Biogeochemical Cycles I