The strength of the lithosphere from geodetic to geologic time-scales

The overarching goal of our studies is to characterise the strength of the lithosphere from geodetic to geologic time-scales and its implications for landscape evolution and mantle dynamics. The strength of the lithosphere allows for the support of high topography in the Tibetan Plateau, controls the formation of rift basin stratigraphic architecture, and modulates the effect of dynamic topography in South East Asia. This year we have quantified how inelastic deformation inflicts stress on Earth, opening a door to understanding the formation of rifted margins like the South China Sea.

Funding Sources: 

  • Earth Observatory of Singapore

Project Years: 

2017
2018

EOS Team: