Results 71 to 80 of about 406 (161)

Partitioning of Iron Between (Mg,Fe)SiO3 Liquid and Bridgmanite

open access: yesGeophysical Research Letters
The evolution of the magma ocean that occupied the early Earth is influenced by the buoyancy of crystals in silicate liquid. At lower mantle pressures, silicate crystals are denser than the iso‐chemical liquid, but heavy elements like iron can cause ...
Francis Dragulet, Lars Stixrude
doaj   +1 more source

Penetration of Warm Slabs Across the 660 km Boundary: The Potential Role of Hydrous Stishovite

open access: yesGeophysical Research Letters
We investigate the phase boundary of hydrous/anhydrous post‐spinel transition at conditions relevant to the 660 km boundary. For the hydrous ringwoodite decomposition, the slope is found to range from negative to positive values depending on the ...
Rabindranath Mondal, Swastika Chatterjee
doaj   +1 more source

In situ determination of crystal structure and chemistry of minerals at Earth's deep lower mantle conditions

open access: yesMatter and Radiation at Extremes, 2017
Recent advances in experimental techniques and data processing allow in situ determination of mineral crystal structure and chemistry up to Mbar pressures in a laser-heated diamond anvil cell (DAC), providing the fundamental information of the ...
Hongsheng Yuan, Li Zhang
doaj   +1 more source

Wetting Behavior of Iron–Carbon Melt in Silicates at Mid-Mantle Pressures With Implications for Earth’s Deep Carbon Cycle

open access: yesFrontiers in Earth Science, 2019
Metallic melt containing iron (Fe) and carbon (C) may be present at depths greater than 250 km inside the Earth. Depending on its wetting behavior, such dense melt may be trapped locally or drain into deep mantle and core.
Junjie Dong   +3 more
doaj   +1 more source

Synthesis of Bridgmanite Using a Multi-Anvil Apparatus

open access: yes
This record contains the detailed information for synthesizing two bridgmanite samples (I1567-1 and S7573) using a multi-anvil apparatus, including starting materials, synthesis method, and major-element compositions.
Lu, Wenhua   +3 more
openaire   +2 more sources

Depth Dependent Deformation and Anisotropy of Pyrolite in the Earth's Lower Mantle

open access: yesGeophysical Research Letters
Seismic anisotropy is a powerful tool to map deformation processes in the deep Earth. Below 660 km, however, observations are scarce and conflicting.
Jeffrey P. Gay   +7 more
doaj   +1 more source

Thermoelastic properties of bridgmanite using deep-potential molecular dynamics

open access: yesPhysical Review B
MgSiO_3-perovskite (MgPv) plays a crucial role in the Earth's lower mantle. This study combines deep-learning potential (DP) with density functional theory (DFT) to investigate the structural and elastic properties of MgPv under lower mantle conditions.
Tianqi Wan   +3 more
openaire   +2 more sources

Dislocation creep may control bridgmanite deformation in the Earth’s lower mantle

open access: yesCommunications Earth & Environment
Seismic anisotropy in the Earth’s lower mantle, particularly around subduction zones, is commonly attributed to deformation by dislocation creep, yet much of the lower mantle appears nearly isotropic.
Longli Guan   +6 more
doaj   +1 more source

High Sodium Solubility in Magnesiowüstite in Iron‐Rich Deep Lower Mantle

open access: yesGeochemistry, Geophysics, Geosystems
(Mg,Fe)O ferropericlase‐magnesiowüstite has been proposed to host the majority of Earth's sodium, but the mechanism and capacity for incorporating the alkali cation remain unclear.
Susannah M. Dorfman   +5 more
doaj   +1 more source

Early-crystalized bridgmanite as a source of primitive noble gases

open access: yes
Abstract Ocean island basalts (OIB) provide a unique window into the deep Earth, with one of the most valuable signals coming from the He and Ne noble gases. The isotopes of these elements point to a “primitive” volatile reservoir in the deep interior that has remained far less degassed than the upper mantle sampled by MORBs.
Yunguo Li   +5 more
openaire   +1 more source

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