Topographic Relief Response to Fluvial Incision in the Central Tibetan Plateau: Evidence From Cosmogenic 10Be
Open Access
- 22 October 2021
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Earth Surface
- Vol. 126 (10)
- https://doi.org/10.1029/2021jf006111
Abstract
No abstract availableKeywords
This publication has 73 references indexed in Scilit:
- Active faulting, mountain growth, and erosion at the margins of the Tibetan Plateau constrained by in situ-produced cosmogenic nuclidesTectonophysics, 2013
- Two-phase growth of high topography in eastern Tibet during the CenozoicNature Geoscience, 2012
- Prolonged seismically induced erosion and the mass balance of a large earthquakeEarth and Planetary Science Letters, 2011
- Spatial distribution of denudation in Eastern Tibet and regressive erosion of plateau marginsTectonophysics, 2010
- A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ18O recordsPaleoceanography and Paleoclimatology, 2005
- The limited influence of glaciations in Tibet on global climate over the past 170 000 yrEarth and Planetary Science Letters, 2002
- Air pressure and cosmogenic isotope productionJournal of Geophysical Research, 2000
- Dynamics of the stream‐power river incision model: Implications for height limits of mountain ranges, landscape response timescales, and research needsJournal of Geophysical Research, 1999
- Modeling fluvial erosion on regional to continental scalesJournal of Geophysical Research, 1994
- Cosmic ray labeling of erosion surfaces: in situ nuclide production rates and erosion modelsEarth and Planetary Science Letters, 1991