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
Uncovering and quantifying the subduction zone sulfur cycle from the slab perspective. [PDF]
Li JL +8 more
europepmc +1 more source
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone. [PDF]
Oyanagi R, Okamoto A.
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Rodingite‐Derived Melt as a Recipe for Ultra‐Calcic Magmas
Abstract Rodingite is a high‐CaO rock formed by Ca‐rich fluid metasomatism on mafic protoliths. It typically occurs within serpentinite and represents an often‐overlooked constituent of the altered oceanic lithosphere that may be subducted into the mantle.
Mingdi Gao +5 more
wiley +1 more source
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
Abstract The mantle transition zone (MTZ; ∼410–660 km depth) is a major reservoir of water and mid‐ocean ridge basalt (MORB)‐like materials, yet how composition and hydration regulate its physical stability remains unclear. Using geodynamical modeling, we examine the joint effect of water content and dense MORB fraction on the density, viscosity, and ...
Zhensheng Wang +6 more
wiley +1 more source
Juxtaposed slab dehydration, decarbonation and seismotectonic variation beneath the Philippine subduction zone based on 3-D modeling. [PDF]
Zhu Y +5 more
europepmc +1 more source
Quantifying the Role of 3D Fault Geometry Complexities on Slow and Fast Earthquakes
Abstract Traditional models of slow slip events (SSEs) oversimplify fault geometry, although imaging shows subduction faults are segmented and complex. We examine how fault interactions control slip behavior using 3D quasi‐dynamic simulations of two parallel faults with uniform rate‐weakening friction accelerated by hierarchical matrices.
J. Cheng +4 more
wiley +1 more source
Abstract Fault‐slip reversals indicate transient stress changes and may illuminate earthquake preparation processes. Here we present high‐resolution observations of sub‐millimetric creep and slip reversals on the Altaquelle Fault, a Quaternary normal fault in the southern Vienna Basin, preceding a regionally significant intraplate earthquake sequence ...
I. Baroň +13 more
wiley +1 more source
Different earthquake nucleation conditions revealed by stress drop and b-value mapping in the northern Chilean subduction zone. [PDF]
Folesky J.
europepmc +1 more source

