Old Web
English
Sign In
Acemap
>
Paper
>
Lithospheric Flow in Tibet: Channelised Flow or Vertically Coupled Deformation?
Lithospheric Flow in Tibet: Channelised Flow or Vertically Coupled Deformation?
2006
Simon L. Klemperer
Keywords:
Thrust tectonics
Craton
Convergent boundary
Tilted block faulting
Geophysics
Isostasy
Open-channel flow
Underplating
Geology
Earth's internal heat budget
Correction
Cite
Save
Machine Reading By IdeaReader
0
References
0
Citations
NaN
KQI
[]