Results 81 to 90 of about 16,900 (220)

Mantle plumes on Venus revisited [PDF]

open access: yes
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

Anomalies of Density, Stresses, and the Gravitational Field in the Interior of Mars

open access: yes, 2012
We determined the possible compensation depths for relief harmonics of different degrees and orders. The relief is shown to be completely compensated within the depth range of 0 to 1400 km.
A. S. Konopliv   +14 more
core   +1 more source

Low-velocity anomaly in the Coral Sea associated with subducting slabs and the Woodlark rift

open access: yesCommunications Earth & Environment
Classical plume models offer insights into intraplate volcanism and seamount chain formation by assuming a cylindrical upwelling of hot materials from the core-mantle boundary.
Ji-hoon Park, Sung-Joon Chang
doaj   +1 more source

Sea floor swells and mantle plumes [PDF]

open access: yes
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

Mantle plumes are oxidised

open access: yesEarth and Planetary Science Letters, 2019
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   +5 more sources

Modeling Anisotropic Signature of Slab‐Induced Mantle Plumes From Thermochemical Piles in the Lowermost Mantle

open access: yesGeophysical Research Letters
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

Long‐Lived Source Heterogeneities in the Galapagos Mantle Plume

open access: yesGeochemistry, Geophysics, Geosystems, 2018
Mantle plume‐derived melts provide a unique glimpse into the chemical heterogeneity of the deep mantle. However, the exact processes involved in forming and sampling lower mantle heterogeneities remain unresolved and thus, require further investigation ...
Esteban Gazel   +6 more
doaj   +1 more source

Depleted mantle plumes [PDF]

open access: yesGoldschmidt2021 abstracts, 2021
Tim Jones, James Day
openaire   +1 more source

Reaching for Ancestral Heritage: Sakha Collections in the Museums of the World

open access: yesMuseum Anthropology, Volume 49, Issue 1, Spring 2026.
ABSTRACT This paper is devoted to the collections of old Sakha objects produced by Indigenous craftsmen in the north of the Russian Empire and now located in many museums around the world. For several centuries, objects representing Sakha material culture were taken away from their place of origin by explorers, scholars, collectors, and missionaries ...
Tatiana Argounova‐Low
wiley   +1 more source

Towards Realistic Progenitors of Core-Collapse Supernovae

open access: yes, 2011
Two-dimensional (2D) hydrodynamical simulations of progenitor evolution of a 23 solar mass star, close to core collapse (about 1 hour, in 1D), with simultaneously active C, Ne, O, and Si burning shells, are presented and contrasted to existing 1D models (
Arnett   +52 more
core   +1 more source

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