Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins. [PDF]
Wang S, Leng W.
europepmc +1 more source
Double volcanic tracks at Hawaii caused by bridgmanite-enriched primordial mantle blobs. [PDF]
Liu H +5 more
europepmc +1 more source
Dual slab stagnation depths controlled by grain-size-induced sporadic low-viscosity zones at around 1000 km depth. [PDF]
Li J, Li K, Li J, Fei H, Hu J.
europepmc +1 more source
Himalayan sub-Moho earthquakes suggest crustal faults trigger eclogitized-drip tectonics. [PDF]
Song X, Klemperer SL.
europepmc +1 more source
How subduction evolution drives sediment-hosted mineralisation along craton edges. [PDF]
Shirmard H +4 more
europepmc +1 more source
Recent Advances in Deep Mantle Rheology
openaire +2 more sources
Waned mantle upwelling contributes to a heavily deformed northern smooth plains on Mercury. [PDF]
Xie J, Zhan Y, Gong S, Huang C, Zhang J.
europepmc +1 more source
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Xu X +14 more
europepmc +1 more source
Mantle rheology, constitution, and convection
Christensen, Ulrich R., Peltier, W. R.
openaire +1 more source
Sublithospheric diamond constraints on the state of deeply subducted slabs. [PDF]
Zhang Q +11 more
europepmc +1 more source

