Results 101 to 110 of about 1,408 (194)

Seamounts off the West Antarctic margin: A case for non-hotspot driven intraplate volcanism

open access: yes, 2014
Highlights: • Marie Byrd Seamounts (MBS) formed off Antarctica at 65-56 Ma in an extensional regime • MBS originate from HIMU-type mantle attached at the base of the Antarctic lithosphere • Continental insulation flow transferred HIMU mantle into the ...
Hauff, Folkmar   +10 more
core   +1 more source

Recycled Oceanic Crust in the Source of the Intraplate Changbaishan‐Tianchi Volcano, China/North Korea

open access: yesGeochemistry, Geophysics, Geosystems
Continental intraplate volcano is an ideal probe to unravel the composition and structure of the deep Earth. The intraplate Changbaishan‐Tianchi volcano was one of the most hazardous eruptions on the Earth's planet. The long‐term activity of this volcano
Yujie Liu   +4 more
doaj   +1 more source

Hydrous Regions of the Mantle Transition Zone Affect Patterns of Intraplate Volcanism

open access: yes, 2022
The Earth’s mantle transition zone (MTZ), located between approximately 410-660 km depth, can store an amount of water equivalent to 2-10 oceans of water, which is transported into the deep mantle by subducting oceanic lithosphere.
Wang, Helene
core  

Phases in fine volcanic ash. [PDF]

open access: yesSci Rep, 2023
Hornby A   +4 more
europepmc   +1 more source

Oceanic intraplate explosive eruptions fed directly from the mantle. [PDF]

open access: yesProc Natl Acad Sci U S A, 2023
DeVitre CL   +9 more
europepmc   +1 more source

Episodic intraplate magmatism fed by a long-lived melt channel of distal plume origin. [PDF]

open access: yesSci Adv, 2023
Naif S   +6 more
europepmc   +1 more source

Anatomy of a post-subduction collision. [PDF]

open access: yesNat Commun
Şengül Uluocak E   +3 more
europepmc   +1 more source

Ancient storage of anomalous mercury isotope signatures in the Earth's transition zone. [PDF]

open access: yesNat Commun
Xu R   +14 more
europepmc   +1 more source

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