Results 51 to 60 of about 19,207 (163)
Slab Geometry and Upper Mantle Flow Patterns in the Central Mediterranean From 3D Anisotropic P-Wave Tomography. [PDF]
Rappisi F +4 more
europepmc +1 more source
The Sunda Plate is a minor tectonic plate bounded by tectonically active convergent boundaries, below which are subducting: the Philippine Sea Plate to the east and the Indo‐Australian Plate to the south and west. It is thus an ideal tectonic setting for
Lingling Wang, Xiaobo He
doaj +1 more source
Evidence for active upper mantle flow in the Atlantic and Indo-Australian realms since the Upper Jurassic from hiatus maps and spreading rate changes. [PDF]
Vilacís B +6 more
europepmc +1 more source
Adjoint traveltime tomography unravels a scenario of horizontal mantle flow beneath the North China craton. [PDF]
Dong X, Yang D, Niu F, Liu S, Tong P.
europepmc +1 more source
Flow directions of rivers are set by the mantle
Large rivers play crucial roles in determining loci of civilisation, natural resources and biodiversity. The positions of their mouths control nutrient and sediment supply to oceans. The paths that rivers take across the Earth’s surface varies considerably with scale. For example, at large scales big North American rivers (e.g.
Lipp, Alex, Roberts, Gareth
openaire +3 more sources
The crystallographic preferred orientation (CPO) of polycrystalline olivine affects both the viscous and seismic anisotropy of Earth's upper mantle with wide geodynamical implications.
Nicholas M. Rathmann +4 more
doaj +1 more source
A large mantle helium anomaly and separate domains of high heat flow are the predominant manifestations of bimodal magmatic activity in the Milford valley.
Stuart F. Simmons, Stefan Kirby
doaj +1 more source
Resistance to mantle flow inferred from the electromagnetic strike of the Australian upper mantle
Seismic anisotropy is thought to result from the strain-induced lattice-preferred orientation of mantle minerals, especially olivine, owing to shear waves propagating faster along the a-axis of olivine crystals than along the other axes. This anisotropy results in birefringence, or 'shear-wave splitting', which has been investigated in numerous studies.
openaire +4 more sources
How crustal deformation responds to complex mantle flow in continental back‐arc settings remains poorly constrained. Here, we develop a Bayesian working‐likelihood approach to estimate crust‐averaged azimuthal anisotropy from P‐wave receiver functions ...
Chunsen Li +5 more
doaj +1 more source
Seismic anisotropy, observed in the lowermost mantle near Large Low‐Shear‐Velocity Provinces (LLSVPs), is likely caused by strong deformation from mantle flow interacting with these regions and/or plume formation.
Poulami Roy +3 more
doaj +1 more source

