受2008年汶川地震后收集的位置数据的约束的计算机建模表明,下地壳的粘性比其下方的上地幔要小。
Tibetan Plateau
Support for a “Jelly Sandwich” Model of the Tibetan Plateau
Computer modeling constrained by positional data collected in the aftermath of the 2008 Wenchuan earthquake indicates the lower crust is less viscous than the upper mantle below it.
A River Ran Through It
The history of river system in southeast Tibet and Indochina reconstructed using the ages of thousands of zircon sand grains in modern and ancient river sediments.
A Landscape Shaped by Wind
High-altitude aeolian research on the Tibetan Plateau offers insights into the past, present, and future.
Dynamics of the Earth's Surface in the Eastern Tibetan Plateau
River erosion increased rapidly following rock uplift events in the plateau approximately 11 million years ago.
