Results 181 to 190 of about 3,661 (237)

Calcium Solubility of Bridgmanite in Subducted Basalt in Earth's Lower Mantle

Geophysical Research Letters, Volume 53, Issue 14, 28 July 2026.
Abstract The calcium solubility in bridgmanite and the resulting abundance of davemaoite under lower‐mantle pressure‐temperature conditions have been under debate following a recent report of extensive calcium dissolution in bridgmanite. We experimentally investigated the calcium solubility in bridgmanite in a basaltic composition at pressures up to ...
Chengwei Zhang, Takashi Yoshino, Elias El Ghazaoui, Stella Chariton, Vitali B. Prakapenka, Luo Li, Yanyao Zhang, Jung‐Fu Lin   +7 more
wiley   +1 more source

Electromagnetic imaging reveals insufficient fluids to explain shallow megathrust creep at the Shumagin Gap. [PDF]

Nat Commun
Li Y, Naif S, Key K, Constable S, Evans RL, Shillington DJ, Bécel A, Cordell D.   +7 more
europepmc   +1 more source

Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions. [PDF]

Proc Natl Acad Sci U S A
Chen S, Wang S, Qi X, Xu M, Yu T, Wang Y, Li B.   +6 more
europepmc   +1 more source

Zinc isotope evidence for extensive carbonate recycling in the Arctic asthenosphere. [PDF]

Nat Commun
Zhang WQ, Ding WW, Liu CZ, Lissenberg CJ, Wang YJ, Zhang T, Tan PC, Zou ZQ, Xu Y, Lu JG, Fang YX, Li JB.   +11 more
europepmc   +1 more source

Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]

Nat Commun
Wolf SG, Huismans RS, Muñoz JA, May DA.
europepmc   +1 more source

Delineating the Central Anatolia Transition Zone (CATZ): Constraints from Integrated Geodetic (GNSS/InSAR) and Seismic Data. [PDF]

Sensors (Basel)
Kutoğlu ŞH, Akgün E, Softa M.
europepmc   +1 more source

Paleoarchean deep crustal hydration and oxidation induced by subduction-driven water recycling. [PDF]

Sci Adv
Zhou D, Ge R, Wilde SA, Collins WJ, Kemp AIS, Lian D, Cai P, Wang X.   +7 more
europepmc   +1 more source

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Subduction zones

Reviews of Geophysics, 2002
Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's 55,000 km of convergent plate margins and are the geodynamic system that builds island arcs.
exaly   +2 more sources

Fluid Processes in Subduction Zones

Science, 1990
Fluids play a critical role in subduction zones and arc magmatism. At shallow levels in subduction zones (<40 kilometers depth), expulsion of large volumes of pore waters and CH 4 -H 2 O fluids produced by diagenetic and low-grade metamorphic reactions affect the thermal and rheological ...
exaly   +3 more sources

Subduction Zones Parameters ☆

2017
Subduction zones are characterized by multiple behaviors, dynamics, or geometries. Most of them results from the complex interplay between various parameters. In this article, we define the most common parameters used by scientists and then mention the studies where (set of) parameters are tested empirically, or experimentally.
Lallemand, Serge, Heuret, Arnauld
openaire   +1 more source