Segmented strain accumulation in the High Himalaya expressed in river channel steepness
Author:
Affiliation:
1. University of Houston, 4800 Calhoun Road, Houston, Texas 77004, USA
2. University of Kansas, 1450 Jaywalk Blvd., Lawrence, Kansas 66045, USA
Publisher
Geological Society of America
Subject
Stratigraphy,Geology
Link
https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/14/3/1131/4181737/1131.pdf
Reference135 articles.
1. Evidence for Pliocene–Quaternary normal faulting in the hinterland of the Bhutan Himalaya;Adams;Lithosphere,2013
2. Constraints on the tectonic and landscape evolution of the Bhutan Himalaya from thermochronometry;Adams;Tectonics,2015
3. In situ development of high-elevation, low-relief landscapes via duplex deformation in the Eastern Himalayan hinterland, Bhutan: Journal of Geophysical Research;Adams;Earth Surface,2016
4. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard;Ader;Journal of Geophysical Research,2012
5. Lithologic and tectonic controls on bedrock channel form at the northwest Himalayan front: Journal of Geophysical Research;Allen;Earth Surface,2013
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