Trabajo presentado en el AGU (American Geophysical Union) Fall Meeting: Advancing Earth and Space Science, celebrado en San Francisco (Estados Unidos), del 12 al 16 de diciembre de 2016Subduction zones show significant variability in shear wave splitting, both above and below the slab, and along-strike. For example, in the Peruvian flat slab region, where the slab has a 3D morphology, shear wave splitting shows complex patterns that indicate that the anisotropic structure varies both laterally and vertically. Above the flat-slab, fast directions measured on shear wave splitting of local S phases are dominantly trench-parallel north of the Nazca Ridge, but become more complicated towards the south as the slab steepens. For SKS phases that sa...
The lowermost mantle-also known as D"-comprises the few hundred kilometres above the core-mantle bou...
Subduction zones are among the most dynamic tectonic environments on Earth. Deformation mechanisms o...
The dynamics of flat subduction, particularly the interaction between a flat slab and the overriding...
[1] Shear-wave splitting observations from many subduction zones show complex patterns of seismic an...
We performed shear wave splitting analyses to investigate seismic anisotropy across the northern ext...
Abstract The dynamics of flat subduction, particularly the interaction between a flat slab and the o...
Knowledge of mantle flow in convergent margins is crucial to unravelling both the contemporary geody...
The Peruvian flat slab is by far the largest region of flat subduction in the world today, but aspec...
Shear wave splitting observations from many subduction zones show complex patterns of seismic anisot...
[1] Much progress has been made over the past several decades in delineating the structure of subduc...
Shear- wave splitting measurements above the mantle wedge of the Mariana(1) and southern Andean(2,3)...
[1] Inferring the circulation of the mantle around subducting plates from surface measurements of sh...
International audienceHow reliable are shear wave splitting measurements as a means of determining m...
The Andean subduction zone is an excellent place to study deformation within a subducting slab as a...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94690/1/ggge1124.pd
The lowermost mantle-also known as D"-comprises the few hundred kilometres above the core-mantle bou...
Subduction zones are among the most dynamic tectonic environments on Earth. Deformation mechanisms o...
The dynamics of flat subduction, particularly the interaction between a flat slab and the overriding...
[1] Shear-wave splitting observations from many subduction zones show complex patterns of seismic an...
We performed shear wave splitting analyses to investigate seismic anisotropy across the northern ext...
Abstract The dynamics of flat subduction, particularly the interaction between a flat slab and the o...
Knowledge of mantle flow in convergent margins is crucial to unravelling both the contemporary geody...
The Peruvian flat slab is by far the largest region of flat subduction in the world today, but aspec...
Shear wave splitting observations from many subduction zones show complex patterns of seismic anisot...
[1] Much progress has been made over the past several decades in delineating the structure of subduc...
Shear- wave splitting measurements above the mantle wedge of the Mariana(1) and southern Andean(2,3)...
[1] Inferring the circulation of the mantle around subducting plates from surface measurements of sh...
International audienceHow reliable are shear wave splitting measurements as a means of determining m...
The Andean subduction zone is an excellent place to study deformation within a subducting slab as a...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94690/1/ggge1124.pd
The lowermost mantle-also known as D"-comprises the few hundred kilometres above the core-mantle bou...
Subduction zones are among the most dynamic tectonic environments on Earth. Deformation mechanisms o...
The dynamics of flat subduction, particularly the interaction between a flat slab and the overriding...