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Velocity and density characteristics of subducted oceanic crust and the origin of lower-mantle heterogeneities [PDF]
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
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Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin [PDF]
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
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Workshop report: Exploring deep oceanic crust off Hawai`i [PDF]
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
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Subducted oceanic crust as the origin of seismically slow lower-mantle structures
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
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Effects of Oceanic Crustal Thickness on Intermediate Depth Seismicity
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
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A Role for Subducted Oceanic Crust in Generating the Depleted Mid‐Ocean Ridge Basalt Mantle
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
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Seismic Formation Fluid Pressure Observations Reveal High Anisotropy of Oceanic Crust
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
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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
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Regional Geophysics of the Caribbean and Northern South America: Implications for Tectonics
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
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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
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