Date: Thursday, April, 3, 2014:
12:30 – 13:30
Place: Techno-Z, GI-lecture room: SC30OG1.107 (Schillerstraße 30, building 14)
Presenter: XIONG Liyang (PhD student from Nanjing
Normal University)
Geomorphometry used in Loess
deposition process investigating and loess landform evolution modeling in the
Loess Plateau of China.
The evolution of loess landforms is largely controlled by the pre-Quaternary
underlying bedrock terrain, which is one of the most important factors in
understanding the formation mechanism of the landforms.
An underlying terrain was simulated together with its geologic information first. And then the loess deposition process was investigated through the comparison between modern terrain and underlying terrain. Finally, we try to numerically modeling the landform evolution process together with the underlying terrain.
An underlying terrain was simulated together with its geologic information first. And then the loess deposition process was investigated through the comparison between modern terrain and underlying terrain. Finally, we try to numerically modeling the landform evolution process together with the underlying terrain.
No comments:
Post a Comment