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Channel debris from landslides serves as the primary material source for debris flows in the arid Daheba Basin, Northeast marginal Tibet Plateau

Crossref DOI link: https://doi.org/10.1007/s11629-025-9908-5

Published Online: 2026-01-14

Published Print: 2026-01

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Du, Cui https://orcid.org/0000-0003-2892-1517
Gu, Yu https://orcid.org/0009-0004-7461-2234
Ma, Chao https://orcid.org/0000-0001-8385-0825
Wu, You https://orcid.org/0009-0003-8123-2427
Lyu, Liqun https://orcid.org/0000-0002-4430-3594
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Text and Data Mining valid from 2026-01-01

Version of Record valid from 2026-01-01
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Article History

Received: 18 June 2025

Revised: 27 September 2025

Accepted: 2 November 2025

First Online: 14 January 2026

Ethics Declaration

: Conflict of Interest: The authors declare no conflict of interest.