Results 101 to 110 of about 1,408 (194)
Seamounts off the West Antarctic margin: A case for non-hotspot driven intraplate volcanism
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
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
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
Specific activities of natural rocks and soils at quaternary intraplate volcanism north of Sana'a, Yemen. [PDF]
Harb S +4 more
europepmc +1 more source
Oceanic intraplate explosive eruptions fed directly from the mantle. [PDF]
DeVitre CL +9 more
europepmc +1 more source
Episodic intraplate magmatism fed by a long-lived melt channel of distal plume origin. [PDF]
Naif S +6 more
europepmc +1 more source
Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere. [PDF]
Spandler C, Merdith AS, Griffin A.
europepmc +1 more source
Anatomy of a post-subduction collision. [PDF]
Şengül Uluocak E +3 more
europepmc +1 more source
Ancient storage of anomalous mercury isotope signatures in the Earth's transition zone. [PDF]
Xu R +14 more
europepmc +1 more source

