Pristine helium from the Karoo mantle plume within the shallow asthenosphere beneath Patagonia
Mantle xenoliths usually represent fragments derived from the depleted and degassed lithospheric mantle with 3He/4He isotope ratios (6 ± 1 RA) lower than those of mid-ocean ridge basalts (8 ± 1 RA).
Tiago Jalowitzki +10 more
doaj +1 more source
Kimberlite genesis from a common carbonate-rich primary melt modified by lithospheric mantle assimilation. [PDF]
Giuliani A +9 more
europepmc +1 more source
LITHOSPHERE MANTLE DENSITY BENEATH THE SIBERIAN CRATON [PDF]
Cherepanova, Yulia, Artemieva, Irina
openaire +2 more sources
Evolution of midplate hotspot swells: Numerical solutions [PDF]
The evolution of midplate hotspot swells on an oceanic plate moving over a hot, upwelling mantle plume is numerically simulated. The plume supplies a Gaussian-shaped thermal perturbation and thermally-induced dynamic support.
Chase, Clement G., Liu, Mian
core +1 more source
Accretion of "young" Phanerozoic subcontinental lithospheric mantle triggered by back-arc extension-the case of the Ivrea-Verbano Zone. [PDF]
Ogunyele AC +4 more
europepmc +1 more source
Cratonic lithospheric mantle: Is anything subducted?
William L. Griffin +1 more
openaire +2 more sources
Himalayan sub-Moho earthquakes suggest crustal faults trigger eclogitized-drip tectonics. [PDF]
Song X, Klemperer SL.
europepmc +1 more source
Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin. [PDF]
Su H, Leng W, Liao J, Brune S.
europepmc +1 more source
Unveiling the metallogenic continuum of an Archean craton. [PDF]
Demmer M, Ezad I, Fiorentini M.
europepmc +1 more source

