Results 151 to 160 of about 40,674 (250)
Geochemical cycling of arsenic in magmatic systems across supercontinent cycles. [PDF]
Cheng Q +7 more
europepmc +1 more source
Abstract Topographic highlands commonly develop along convergent plate boundaries through long‐term processes such as subduction and continental collision. However, the pre‐Cenozoic mountain‐building history of deep‐time orogenic systems in northeastern Pangaea remains poorly constrained due to later tectonic overprinting and denudation.
Heng Peng +9 more
wiley +1 more source
Paired magnetic susceptibility and geochemistry of young volcanism in Iceland and Tengchong, China. [PDF]
Zhang Y, Mitchell RN.
europepmc +1 more source
Shallow Creep in the Leaky Stress Shadow of Locked Zones of Subduction Megathrust
Abstract In some subduction zones such as Nankai, creeping of the shallow part of the megathrust in the stress shadow of deeper locked zones is detected by seafloor geodetic measurements and/or reflected by slow earthquakes (SEQs). Here we explain that shallow creep occurs in the stress shadow for two reasons: (a) prolonged afterslip and (b) a leaky ...
Kelin Wang, Yajing Liu, Tianhaozhe Sun
wiley +1 more source
Oxidized sediment recycling as a driver for postsubduction porphyry copper formation. [PDF]
Yang Z +7 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
Abiotic polycyclic aromatic hydrocarbons originating from the sub-oceanic mantle. [PDF]
Mitsukawa I +13 more
europepmc +1 more source
Hydraulic Control of the Foreshocks and Mainshock of the 2017 Valparaíso, Chile, Earthquake
Abstract Slow‐slip events (SSE) are a key mode of aseismic deformation and can enhance fault permeability through fracturing, enabling fluid migration from the overpressured oceanic crust to the plate interface. Whether the resulting poroelastic stress changes promote seismicity and larger megathrust events, however, remains unclear.
Carlos Peña +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
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

