(Q58110255)

Has focused denudation sustained active thrusting at the Himalayan topographic front?

inferred from page(s)

published in

Nature

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volume

434

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issue

7036

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page(s)

1008-1011

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cites work

1 reference

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Quaternary deformation, river steepening, and heavy precipitation at the front of the Higher Himalayan ranges

21 January 2018

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Decoupling of erosion and precipitation in the Himalayas.

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Denudation rates determined from the accumulation of in situ-produced 10Be in the luquillo experimental forest, Puerto Rico

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Large-scale erosion rates from in situ-produced cosmogenic nuclides in European river sediments

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Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas

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GPS measurements of present-day convergence across the Nepal Himalaya

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Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation

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Modeling mountain building and the seismic cycle in the Himalaya of Nepal

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7 January 2021

Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal

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7 January 2021

Fluvial incision and tectonic uplift across the Himalayas of central Nepal

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Seismotectonics of the Nepal Himalaya from a local seismic network

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Tectonics of the Himalaya and southern Tibet from two perspectives

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Stratigraphy, structure, and tectonic evolution of the Himalayan fold-thrust belt in western Nepal

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7 January 2021

ROCK TO SEDIMENT—SLOPE TO SEA WITH10BE—RATES OF LANDSCAPE CHANGE

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7 January 2021

Erosional equilibrium and disequilibrium in the Sierra Nevada, inferred from cosmogenic 26Al and 10Be in alluvial sediment

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7 January 2021

Estimating Rates of Denudation using Cosmogenic Isotope Abundances in Sediment

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Continuous Snow and Rain Data at 500 to 4400 m Altitude near Annapurna, Nepal, 1999–2001

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7 January 2021

Southward extrusion of Tibetan crust and its effect on Himalayan tectonics

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