Results 71 to 80 of about 1,684 (203)
Abstract From oxic atmosphere to metallic core, the Earth's components are broadly stratified with respect to oxygen fugacity. A simple picture of reducing oxygen fugacity with depth may be disrupted by the accumulation of oxidised crustal material in the deep lower mantle, entrained there as a result of subduction. While hotspot volcanoes are fed by
Moussallam, Yves +9 more
openaire +4 more sources
Deep mantle plumes and an increasing Earth radius
Recent space geodetic and gravimetric studies have given indications that the Earth's radius is increasing at 0.1–0.4 mm yr−1 at present. Seismic studies have also shown that earthquakes alone could be causing the radius to increase at 0.011–0.06 mm yr−1.
Matthew R. Edwards
doaj +1 more source
Abstract The Cenozoic convergence between the Indian and Asian plates has driven large‐scale mantle convection that interacts with both plates. Understanding this convergence benefits from clear imaging of the lithosphere‐asthenosphere boundary (LAB).
Yiming Bai +12 more
wiley +1 more source
Seismic anisotropy, observed in the lowermost mantle near Large Low‐Shear‐Velocity Provinces (LLSVPs), is likely caused by strong deformation from mantle flow interacting with these regions and/or plume formation.
Poulami Roy +3 more
doaj +1 more source
Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation. [PDF]
Doucet LS, Li ZX, Gamal El Dien H.
europepmc +1 more source
ABSTRACT Trauma and loss constitute recurring themes in both Murakami's fictional and non‐fictional writing. In the short story Tony Takitani, Murakami portrays a father and son confronting trauma and loss in the aftermath of the Second World War and the nuclear devastation of Japan.
David Potik
wiley +1 more source
Noble gases confirm plume-related mantle degassing beneath Southern Africa
Southern Africa is characterised by unusually elevated topography and abnormal heat flow. This can be explained by thermal perturbation of the mantle, but the origin of this is unclear.
S. M. V. Gilfillan +10 more
doaj +1 more source
Major and trace element compositions of basaltic lavas from western margin of central main Ethiopian rift: enriched asthenosphere vs. mantle plume contribution. [PDF]
Meshesha D, Chekol T, Negussia S.
europepmc +1 more source
Loess Studies in Aotearoa New Zealand
Loess in Aotearoa New Zealand (ANZ) has been studied since its first documented recognition (on Banks Peninsula) in 1878 by Julius von Haast. A decade later, John Hardcastle revealed that southern ANZ loess was both glacial in origin and contained signals of past climates.
Brent V. Alloway +4 more
wiley +1 more source
Thermal anomalies within the lithosphere are an important manifestation of mantle plume–lithosphere interaction. Early studies primarily concentrated on the presence of the Hainan plume and its surface responses, with comparatively little research ...
Huihui Zhang, Lijuan He, Yaqi Wang
doaj +1 more source

