Results 201 to 210 of about 63,820 (273)
Abstract Alaska's tectonic complexity makes it ideal for probing upper mantle deformation. We present a 3D shear‐wave anisotropy model obtained by inverting 7,985 SKS splitting intensity measurements from 261 broadband stations using 941 events from 2000 to 2023.
Yi Lin, Manuele Faccenda, Li Zhao
wiley +1 more source
An inhomogeneous across-slab conduit controlled by intraslab stress heterogeneity in the Nankai subduction zone. [PDF]
Otsubo M +3 more
europepmc +1 more source
Abstract The Northeastern (NE) Tibet, as the front of plateau growth, widely absorbs northeastward extrusion, leading to significant uplift and forming a basin‐mountain tectonic framework. However, it remains unclear how the crust of NE Tibet deformed in response to the far‐field effects of the India‐Eurasia collision.
Ruo‐Jie Li +4 more
wiley +1 more source
Abstract The tropical Indian Ocean (IO) exhibits persistent biases in sea surface temperature (SST) climatology across Coupled Model Intercomparison Project Phase 6 (CMIP6) models, particularly during boreal winter. These biases manifest as a meridional dipole with warm SSTs in northern tropics and cool SSTs in south.
Guangli Zhang +4 more
wiley +1 more source
Crustal CO2 contribution to subduction zone degassing recorded through calc-silicate xenoliths in arc lavas. [PDF]
Whitley S +5 more
europepmc +1 more source
Permeability Enhancement by Slow Faulting Under High Pore Fluid Pressure
Abstract The morphology of fault zones formed by slow faulting is markedly different from that of brittle faulting. In this study, we quantify the three‐dimensional (3D) pore distribution and permeability structures of two rock samples that have been deformed to failure by slow and brittle faulting, respectively.
Tommaso Mandolini +3 more
wiley +1 more source
Abstract The Sagaing Fault (SF) accommodates major plate motion in Myanmar, yet large earthquakes along it have rarely been captured by modern geodetic and seismic observations. The 2025 Sagaing earthquake generated an exceptionally long rupture (∼535 km), offering a rare opportunity to investigate rupture dynamics along continental transform fault. We
Zhenjiang Liu +8 more
wiley +1 more source
Subduction zone forearc serpentinites as incubators for deep microbial life. [PDF]
Plümper O +7 more
europepmc +1 more source
Abstract During the early Cenozoic greenhouse period, counterintuitive contractions in tropical Pacific oxygen‐deficient zones have been linked to enhanced deep‐ocean ventilation, yet direct geological evidence remains limited. Here we present molybdenum (Mo) isotopic records from International Ocean Discovery Program Site U1509.
Xiaowen Liu +8 more
wiley +1 more source
Nitrogen recycling at the Costa Rican subduction zone: The role of incoming plate structure. [PDF]
Lee H +5 more
europepmc +1 more source

