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The Suwalong paleolandslide is located in the Batang–Zhongza reach of the upper Jinsha River, at the southeast margin of the Tibetan Plateau where tectonic activity is very strong, and has formed a great deal of large paleolandslides or their relicts. The relict deposits that have been exposed around the Suwalong paleolandslide provide an opportunity to understand the formation process and potential...
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