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Velocity and density characteristics of subducted oceanic crust and the origin of lower-mantle heterogeneities [PDF]

open access: yesNature Communications, 2020
Seismology is a powerful tool to investigate Earth’s interior. Here, the authors combine numerical approaches with experimental results from previous studies to show a depth dependent behaviour of seismic waves in subducted oceanic crust in Earth’s ...
Wenzhong Wang   +5 more
doaj   +2 more sources

Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin [PDF]

open access: yesNature Communications
The Continent-Ocean Transition (COT) in the young Tyrrhenian basin documents mantle exhumation punctuated with multiple episodes of discrete oceanic crust formation.
Hao Su, Wei Leng, Jie Liao, Sascha Brune
doaj   +2 more sources

Workshop report: Exploring deep oceanic crust off Hawai`i [PDF]

open access: yesScientific Drilling, 2021
For more than half a century, exploring a complete sequence of the oceanic crust from the seafloor through the Mohorovičić discontinuity (Moho) and into the uppermost mantle has been one of the most challenging missions of scientific ocean drilling. Such
S. Umino   +23 more
doaj   +1 more source

Subducted oceanic crust as the origin of seismically slow lower-mantle structures

open access: yesProgress in Earth and Planetary Science, 2020
Mantle tomography reveals the existence of two large low-shear-velocity provinces (LLSVPs) at the base of the mantle. We examine here the hypothesis that they are piles of oceanic crust that have steadily accumulated and warmed over billions of years. We
Timothy D. Jones   +4 more
doaj   +1 more source

Effects of Oceanic Crustal Thickness on Intermediate Depth Seismicity

open access: yesFrontiers in Earth Science, 2020
The occurrence of intermediate depth seismicity (70–300 km) is commonly attributed to the dehydration of hydrous phases within the downgoing oceanic plate.
Lara S. Wagner   +4 more
doaj   +1 more source

A Role for Subducted Oceanic Crust in Generating the Depleted Mid‐Ocean Ridge Basalt Mantle

open access: yesGeochemistry, Geophysics, Geosystems, 2020
The composition of Earth's mantle, continental crust, and oceanic crust continuously evolve in response to the dynamic forces of plate tectonics and mantle convection.
Jonathan M. Tucker   +3 more
doaj   +1 more source

Seismic Formation Fluid Pressure Observations Reveal High Anisotropy of Oceanic Crust

open access: yesGeophysical Research Letters, 2021
Fractures and faults in igneous oceanic crust affect hydrothermal circulation and hydration of the oceanic plates. Seismic observations have provided information about lithospheric fabrics, but direct measurements of oceanic crust’s elastic properties ...
Tianhaozhe Sun   +2 more
doaj   +1 more source

Constraints on the structure of the oceanic crust of the Tamu Massif by teleseismic P-wave coda autocorrelation

open access: yesFrontiers in Earth Science, 2023
The Tamu Massif, considered the biggest single volcano on Earth, was formed by the accumulation of enormous amounts of magma erupting to the surface. It is the largest and oldest seamount in Shatsky Rise, which is the third largest oceanic plateau on ...
Fucong Xu   +9 more
doaj   +1 more source

Regional Geophysics of the Caribbean and Northern South America: Implications for Tectonics

open access: yesGeochemistry, Geophysics, Geosystems, 2022
The Caribbean plate is an enclosed oceanic basin whose formation and evolution are controversial. In the most commonly accepted model, the Caribbean plate is mainly composed of the Caribbean Large Igneous Province (CLIP) and the buoyant characteristic of
Carol V. Barrera‐Lopez   +2 more
doaj   +1 more source

Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano

open access: yesEarth, Planets and Space, 2020
To explore a local relationship between geological structures and the occurrence of very-low-frequency earthquakes (VLFEs), a particular class of slow earthquakes with characteristic periods of 10–100 s, we investigated three-dimensional (3D) structural ...
Kazuya Shiraishi   +4 more
doaj   +1 more source

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