Results 181 to 190 of about 2,100,958 (324)
Abstract Since the Mesozoic, much of the eastern China lithosphere was removed through thermo‐mechanical erosion and delamination, yet the effects on the overlying crust remain unclear. The Tanlu Fault Zone (TLFZ), the region's largest lithosphere‐scale weakness, offers a natural laboratory to assess crustal responses to lithospheric destruction.
Yuqi Zhu +5 more
wiley +1 more source
Coeval upper crustal extension and surface uplift in the Central Taurides (Türkiye) above the Cyprus Subduction Zone. [PDF]
Aykut T +4 more
europepmc +1 more source
Abstract Unraveling the surface deformation and fault kinematics during the seismic cycle is crucial for understanding earthquake physics. Herein, we use geodetic and seismic observations to quantify the interseismic coupling, coseismic rupture, and postseismic afterslip associated with the 2025 Mw 8.8 Kamchatka earthquake.
Yang Xiao +8 more
wiley +1 more source
Author Correction: Control of slab tears and slab flat wedging on volcanism in the Alaska subduction zone. [PDF]
Hu Y, Liu C, Wang Z, Zhao F.
europepmc +1 more source
The 2025 Mw 8.8 Kamchatka Megathrust: A Rapid Recurrence With Complex Heterogeneous Rupture
Abstract On 29 July 2025, a Mw 8.8 earthquake struck Kamchatka, ∼50 km from the 1952 Mw 9.0 megathrust hypocenter, exhibiting a comparable aftershock zone. We resolve the kinematic rupture process and slip distribution by combining teleseismic waveforms with high‐quality tsunami data.
Junpeng Li, Zhe Jia
wiley +1 more source
Abstract A M5.9 earthquake occurred on 29 March 2024, offshore near the Strofades Islands, in the western Hellenic Subduction System. Here we present high‐precision earthquake locations and focal mechanisms that suggest the rupture of a NNE‐SSW striking, left‐lateral strike‐slip fault.
G. M. Bocchini +8 more
wiley +1 more source
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone. [PDF]
Oyanagi R, Okamoto A.
europepmc +1 more source
Timothy E. Keenan +6 more
semanticscholar +1 more source

