Coseismic Debris Remains in the Orogen Despite a Decade of Enhanced Landsliding-Reference-Cited by-同舟云学术

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Coseismic Debris Remains in the Orogen Despite a Decade of Enhanced Landsliding

Published:2021-10-07 Issue:19 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Dai Lanxin¹,Scaringi Gianvito²^ORCID,Fan Xuanmei¹^ORCID,Yunus Ali P.¹,Liu‐Zeng Jing³,Xu Qiang¹,Huang Runqiu¹

Affiliation:

1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection Chengdu University of Technology Chengdu China

2. Faculty of Science Institute of Hydrogeology Engineering Geology and Applied Geophysics Charles University Prague Czech Republic

3. Institute of Surface‐Earth System Science Tianjin University Tianjin China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL095850

Reference62 articles.

1. Stochastic forcing of sediment supply to channel networks from landsliding and debris flow

2. Pulsed carbon export from mountains by earthquake-triggered landslides explored in a reduced-complexity model

3. Seismic cycles, earthquakes, landslides and sediment fluxes: Linking tectonics to surface processes using a reduced-complexity model

4. Earthquake-triggered increase in sediment delivery from an active mountain belt

5. Initiation and Runout of Post‐Seismic Debris Flows: Insights From the 2015 Gorkha Earthquake

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4. Identifying potential debris flow hazards after the 2022 Mw 6.8 Luding earthquake in southwestern China;Bulletin of Engineering Geology and the Environment;2024-05-20

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