Results 201 to 210 of about 74,600 (292)
Coupling between crustal uplift and magnetic demagnetization in the Tarim Basin. [PDF]
Xu B, Zhao C, Zhang L, Yu P.
europepmc +1 more source
Layered Seismic Anisotropy and Tectonics of the Anatolian Plate
Abstract Anatolian tectonics are associated with slab retreat in the west and gravitational potential energy and continental collision in the east, leading to westward motion of Anatolia relative to Eurasia, partially accommodated on the North and East Anatolian transform faults.
Chuanming Liu +4 more
wiley +1 more source
Geochemical fingerprinting of plume in Suswa silicic volcanics, Kenya rift. [PDF]
Hong LB +5 more
europepmc +1 more source
Abstract We present a high‐resolution local earthquake tomography model that constrains the distribution of hydration and dehydration processes within the subducting Nazca slab beneath Northern Chile. We image a distinct downdip transition from high Vp/Vs (∼1.75) over low Vp/Vs (∼1.65) to a homogeneously high Vp/Vs slab at depths of ≥ ${\ge} $85 km ...
Nazia Hassan, Christian Sippl
wiley +1 more source
Average physical structure of cratonic lithosphere, from thermodynamic inversion of global surface-wave data. [PDF]
Xu Y, Lebedev S, Fullea J.
europepmc +1 more source
Impact of Mantle Velocity Uncertainty on Receiver‐Function Imaging of the Transition Zone
Abstract Seismological estimates of the 400‐km and 670‐km mantle discontinuities (d400 and d670) are crucial for understanding the thermochemical structure and dynamics of the mantle transition zone (MTZ). However, artifacts from using ray theory and uncertainties in mantle velocity structure can affect topographic mapping of these boundaries.
Carlos A. M. Chaves +2 more
wiley +1 more source
Geodynamics of a global plate reorganization from topological data analysis. [PDF]
Janin A +3 more
europepmc +1 more source
Abstract The Southern Array for the Lithosphere and Uplift of Taiwan Experiment (SALUTE) provides a new window into the subduction‐collision transition zone in southern Taiwan, where the Eurasian Plate‐Luzon Arc convergence drives intense orogeny and crustal deformation. Using dense P‐ and S‐wave spectral amplitude data recorded by SALUTE and a quality
Yu‐Pin Lin +5 more
wiley +1 more source
Bilateral Loa-Kea trends of the Hawaiian Islands caused by the bottom-up splitting of plume conduit. [PDF]
Zhang J, Hu J, Wang K.
europepmc +1 more source

