Results 111 to 120 of about 120,010 (213)
Ultra‐Low Velocity Zone Beneath the Atlantic Near St. Helena
There are various hotspots in the Atlantic Ocean, which are underlain by mantle plumes that likely cross the mantle and originate at the core‐mantle boundary. We use teleseismic core‐diffracted shear waves to look for an Ultra‐Low Velocity Zone (ULVZ) at
Sefira Davison +3 more
doaj +1 more source
The Origin of Carbonate Magmas Predating and Accompanying Main‐Phase LIPs Eruptions
Some large igneous provinces (LIPs) are associated with precursory carbonatite eruptions. Models for precursory carbonatites invoking partial melting of a carbonate metasomatized lithosphere appear implausible, given the long time needed for heat ...
Cinzia G. Farnetani, Mark A. Richards
doaj +1 more source
Recycled Components in Mantle Plumes Deduced From Variations in Halogens (Cl, Br, and I), Trace Elements, and 3He/4He Along the Hawaiian-Emperor Seamount Chain. [PDF]
Broadley MW +4 more
europepmc +1 more source
Deep mantle plumes feeding periodic alignments of asthenospheric fingers beneath the central and southern Atlantic Ocean. [PDF]
Munch FD +3 more
europepmc +1 more source
Geophysical hotspots have been attributed to partially molten asthenosphere, fertile blobs, small-scale convection and upwellings driven by core heat. Most are short-lived or too close together to be deeply seated, and do not have anomalous heat flow ...
Anderson, Don L., Natland, James H.
core
Bilateral Loa-Kea trends of the Hawaiian Islands caused by the bottom-up splitting of plume conduit. [PDF]
Zhang J, Hu J, Wang K.
europepmc +1 more source
Pulsation of mantle plumes [PDF]
V. P. Trubitsyn, M. N. Evseev
openaire +1 more source
Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere. [PDF]
Spandler C, Merdith AS, Griffin A.
europepmc +1 more source

