Post‐Miocene Erosion in Central Nepal Controlled by Midcrustal Ramp Position, Duplex Growth, and Dynamically Maintained Elastic Strain
Author:
Affiliation:
1. Department of Earth and Atmospheric Sciences University of Houston Houston TX USA
2. Now at Department of Geological Sciences University of Texas at San Antonio San Antonio TX USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006291
Reference99 articles.
1. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard
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3. Evaluation of precipitation data sets along the Himalayan front
4. Tectonothermal evolution of the Lesser Himalaya, Nepal: Constraints from 40Ar/39Ar ages from the Kathmandu Nappe
5. Himalayan earthquakes: a review of historical seismicity and early 21st century slip potential
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1. Duplex kinematics reduces both frontal advance and seismic moment deficit in the Himalaya;Geology;2022-07-11
2. Megathrust Heterogeneity, Crustal Accretion, and a Topographic Embayment in the Western Nepal Himalaya: Insights from the Inversion of Thermochronological Data;2022-07-03
3. Megathrust Heterogeneity, Crustal Accretion, and a Topographic Embayment in the Western Nepal Himalaya: Insights From the Inversion of Thermochronological Data;Tectonics;2022-07
4. Spatially focused erosion in the High Himalaya and the geometry of the Main Himalayan Thrust in Central Nepal (85°E) from thermo-kinematic modeling of thermochronological data in the Gyirong region (southern China);Tectonophysics;2022-07
5. Coupled Rapid Erosion and Foreland Sedimentation Control Orogenic Wedge Kinematics in the Himalayan Thrust Belt of Central Nepal;Journal of Geophysical Research: Solid Earth;2021-05
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