The transition from crustal compression and strike-slip faulting ... subduction zones may themselves be transformed to other types of plate boundary. For example, when India collided with Asia ...
Where convection currents push plates together, destructive plate boundaries (margins) are formed. Constructive plate margins close constructive plate marginAn area where two tectonic plates are ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results
Feedback