Results 141 to 150 of about 38,766 (189)

Little to no active faulting likely at Europa's seafloor today. [PDF]

Nat Commun
Byrne PK, Dawson HG, Klimczak C, Regensburger PV, Crane KT, Catalano JG, Elder CM, Foley BJ, German CR, Green AP, Hemingway DJ, Melwani Daswani M, Panning MP, Randolph-Flagg N, Sherwood Lollar B, Skemer P, Vance SD, Wiens DA.   +17 more
europepmc   +1 more source

Discovery of Cenozoic magmatic ridges and tectonics off northern Victoria Land provides new insights into the geodynamics of the Antarctic margin. [PDF]

Sci Rep
Civile D, Crispini L, Ruppel A, Ferrante GM, Morelli D, Accettella D, Accaino F, Locatelli M, Volpi V, Busetti M, Armadillo E, Läufer A.   +11 more
europepmc   +1 more source

Highly oxidized intraplate basalts and deep carbon storage. [PDF]

Sci Adv
Dong XH, Wang SJ, Wang W, Huang S, Li QL, Liu C, Gao T, Li S, Wu S.   +8 more
europepmc   +1 more source

Water-induced bridgmanite coarsening may produce highly viscous lower mantle seismic anomalies. [PDF]

Natl Sci Rev
Lyu Y, Fei H, Chakraborti A, Ballmer M, Faul U, Zhou S, Yang Y, Liu J, Xu F, Fu S, Zhang B, Xia Q, Katsura T.   +12 more
europepmc   +1 more source

On the plate velocity scaling break. [PDF]

Sci Rep
Zaccagnino D, Cuffaro M, Ficini E, Doglioni C.   +3 more
europepmc   +1 more source

The origin of intraplate volcanism on the New Zealand microcontinent Zealandia

openaire   +2 more sources

Hafnium isotopic variations in East Atlantic intraplate volcanism

, 2009
openaire   +1 more source

Intraplate Volcanism Originating From Upwelling Hydrous Mantle Transition Zone [PDF]

Nature, 2020
Most magmatism occurring on Earth is conventionally attributed to passive mantle upwelling at mid-ocean ridges, to slab devolatilization at subduction zones, or to mantle plumes. However, the widespread Cenozoic intraplate volcanism in northeast China1–3
Manuele Faccenda, Jianfeng Yang
exaly   +2 more sources

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Controls on Volcanism at Intraplate Basaltic Volcanic Fields

Earth and Planetary Science Letters, 2017
A broad range of controlling mechanisms is described for intraplate basaltic volcanic fields (IBVFs) in the literature. These correspond with those relating to shallow tectonic processes and to deep mantle plumes. Accurate measurement of the physical parameters of intraplate volcanism is fundamental to gain an understanding of the controlling factors ...
Jozua van Otterloo, Laurent Ailleres, Peter Graham Betts   +2 more
exaly   +2 more sources

The Mechanisms Underpinning Cenozoic Intraplate Volcanism in Eastern Australia: Insights From Seismic Tomography and Geodynamic Modeling [PDF]

Geophysical Research Letters, 2017
Cenozoic intraplate volcanism is widespread throughout much of eastern Australia and manifests as both age‐progressive volcanic tracks and non‐age‐progressive lava fields. Various mechanisms have been invoked to explain the origin and distribution of the
Simone Pilia, Nicholas Rawlinson, Rhodri Davies   +2 more
exaly   +6 more sources