Results 211 to 220 of about 120,399 (317)
Subduction rates and volumes for the southern Indian Ocean thermocline [PDF]
Johannes Karstensen, Detlef Quadfasel
openalex
Inferring Long‐Term Tectonic Uplift Patterns From Bayesian Inversion of Fluvially‐Incised Landscapes
Abstract Earth surface processes encode the combined forcing of tectonics and climate in topography. Separating their contributions is essential for using landscapes as quantitative records of crustal deformation. Here, we develop a method to invert non‐dimensionalized, spatially variable fields of long‐term rock uplift and rock erodibility from ...
Bar Oryan +4 more
wiley +1 more source
Role of plate convergence rate in shaping earthquake recurrence in subduction zones. [PDF]
Ray S +4 more
europepmc +1 more source
Abstract Martian magmas compositionally resemble those from terrestrial continental hotspot magmatic suites, characterized by low OH and high Cl and S contents. The magmatic gases exsolved from such magmas transport a variety of metal complexes and, upon cooling, precipitate vapor‐deposits into vugs and fractures within rocks and on the surfaces of ...
N. Zimmermann, M. Safari, H. Nekvasil
wiley +1 more source
Secondary acceleration of slip fronts driven by slow slip event coalescence in subduction zones. [PDF]
Wang J +7 more
europepmc +1 more source
On the dynamics of subduction and the effect of subduction zones on mantle convection
Subduction is one of the principal surface expressions of mantle convection and it represents a key ingredient of global geodynamics. It affects Earth processes ranging from the generation of mega-earthquakes and explosive volcanoes at thesurface to the recycling of volatile species back into the deep interior.
openaire +1 more source
Abstract Hydroclimatic extremes such as droughts and floods severely impact global livelihoods, economies, and ecosystems, yet their attribution remains challenging. This study evaluates global Terrestrial Water Storage (TWS) extremeness and climate linkages using GRACE and GRACE‐FO data from 2002 to 2024.
Ashraf Rateb +3 more
wiley +1 more source
Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt. [PDF]
Li H, Yang Z, Lu Y, Hou Z.
europepmc +1 more source
Structural Controls on Splay Fault Rupture Dynamics During Cascadia Megathrust Earthquakes
Abstract Great subduction earthquakes (Mw ≥ 8.0) can generate devastating tsunamis by rapidly displacing the seafloor and overlying water column. These potentially tsunamigenic seafloor offsets result from coseismic fault slip and deformation beneath or within the accretionary wedge. The mechanics of these shallow rupture phenomena and their dependence
J. Biemiller +8 more
wiley +1 more source
Pore-pressure diffusion controls upper-plate aftershocks of the 2014 Iquique earthquake. [PDF]
Peña C +7 more
europepmc +1 more source

