Tectonic geomorphology, active tectonics and lower crustal channel flow hypothesis of the southeastern Tibetan Plateau

We use high-resolution SRTM DEMs to quantify the large scale topography and geomorphology in southeastern margin of the Tibetan Plateau. The southeastern plateau region is characterized as 'negative topography', i.e., a topography where there is an inverse or negative correlation between e...

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Veröffentlicht in:Dizhi kexue 2009-10, Vol.44 (4), p.1227-1255
Hauptverfasser: Liu, Jing, Zeng, Lingsen, Ding, Lin, Tapponnier, P, Gaudemer, Y, Wen, Li, Xie, Kejia
Format: Artikel
Sprache:chi
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