Results 101 to 110 of about 27,251 (208)
New helium isotope data for basalt glasses from the Gulf of Tadjoura and Gulf of Aden reveal a mantle plume signal that has 3He/4He up to 17 RA. In the Gulf of Aden, plume helium is detectable ∼380 km from the Afar triple junction, up to the Shukra El ...
D. W. Graham, P. J. Michael
doaj +1 more source
Seafloor evidence for pre-shield volcanism above the Tristan da Cunha mantle plume. [PDF]
Geissler WH +8 more
europepmc +1 more source
The mechanisms and processes of interaction between paleo-subducted slabs and mantle plumes are not well understood, primarily due to the challenges associated with direct observation. The Leiqiong Area (LQA), located in the northwestern South China Sea (
Jin Xu +13 more
doaj +1 more source
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
Dynamics of mantle plumes [PDF]
Mantle plumes are a link between different scales in the Earth’s mantle: They are an important part of large-scale mantle convection, transporting material and heat from the core-mantle boundary to the surface, but also affect processes on a smaller scale, such as melt generation and transport and surface magmatism.
openaire
Mantle Plume‐Lithosphere Interactions Beneath the Emeishan Large Igneous Province
The formation of large igneous provinces (LIPs) has been widely believed to be linked to mantle plume activity. However, how the plume modifies the overlying lithosphere, particularly its compositional structure, remains uncertain.
Anqi Zhang +4 more
doaj +1 more source
Sea floor swells and mantle plumes [PDF]
Most of the intraplate oceanic hot spots are located on the crest of broad topographic swells in the sea floor. These swells have Gaussian shaped profiles, with up to 1.6 km of relief and half widths of 200 to 300 km.
Olson, P.
core +1 more source
Imaging the Galápagos mantle plume with an unconventional application of floating seismometers. [PDF]
Nolet G +10 more
europepmc +1 more source
Mantle plumes on Venus revisited [PDF]
The Equatorial Highlands of Venus consist of a series of quasicircular regions of high topography, rising up to about 5 km above the mean planetary radius.
Kiefer, Walter S.
core +1 more source

