P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its geological framework and initial growth were fundamentally the result of multiple, previous …
Variable morphologies of subducting slabs are observed in tomographic images of the mantle transition zone (MTZ), where slabs appear to stagnate in the MTZ or enter the lower …
K Tao, SP Grand, F Niu - Geochemistry, Geophysics …, 2018 - Wiley Online Library
To better understand the subsurface behavior of subducting slabs and their relation to the tectonic evolution of the overriding plate, we conduct a full waveform inversion on a large …
We discuss the relationships between Andean shortening, plate velocities at the trench, and slab geometry beneath South America. Although some correlation exists between the …
Transition zone slab deformation influences Earth's thermal, chemical, and tectonic evolution. However, the mechanisms responsible for the wide range of imaged slab …
WP Schellart, L Moresi - Journal of Geophysical Research …, 2013 - Wiley Online Library
We present numerical subduction models to investigate overriding plate deformation at subduction zones. All models show forearc shortening, resulting predominantly from shear …
Improved constraints on lower-mantle composition are fundamental to understand the accretion, differentiation, and thermochemical evolution of our planet. Cosmochemical …
G Zhu, Y Chen, D Jiang, S Lin - Tectonophysics, 2015 - Elsevier
The Yunmengshan metamorphic core complex (YMMCC) is situated in the northern part of the eastern North China Craton (NCC). The main structures in the YMMCC area include the …
The building of the Andes results from the subduction of the oceanic Nazca plate underneath the South American continent,. However, how and why the Andes and their …