About: Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

Facets (new session)
Description
Metadata
Settings
- owl:sameAs
- Inference Rule:

About: Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity Goto Sponge NotDistinct Permalink

An Entity of Type : wikibase:Item, within Data Space : wikidata.demo.openlinksw.com associated with source document(s)

scientific article published in Nature

Attributes	Values
rdf:type	Item
description	artículu científicu (ast) wetenschappelijk artikel (nl) article publié dans la revue scientifique Nature (fr) scientific article published in Nature (en) im April 1998 veröffentlichter wissenschaftlicher Artikel (de) наукова стаття, опублікована в Nature у квітні 1998 (uk)
publication date	wds:Q59054557-66779CD0-0CA7-4356-B9FB-A22C338B59CB
publication date	1998-04-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59054557-2280B58A-8FAF-4280-AA56-D26B2936714C
language of work or name	English
exact match	wds:Q59054557-D833301D-3232-415F-B4E3-07E119CF41BC
exact match	https://scigraph.springernature.com/pub.10.1038/33663
cites work	wds:Q59054557-087F3A91-1C52-4F4A-A0F3-F0F2B557FD9F wds:Q59054557-24493C5A-C4B8-41DF-9513-78F329B863BE wds:Q59054557-5AEA7E96-87E2-441D-B064-C9F44E8BF77A wds:Q59054557-6E2FEF3D-238C-4FA3-90C3-F561D8066DDC wds:Q59054557-95480D6A-DCD6-41AD-9177-7018A15517D0 wds:Q59054557-A93B6413-F736-4ECC-92FF-72702208E00A wds:Q59054557-B257F2A2-BD35-494B-B17A-E1E7429C26DB wds:Q59054557-D2E77B02-2DC8-4EE4-BBCD-26662CCDBFA3 wds:Q59054557-E5841B07-FFF7-4439-AD0D-9B6A3D14A583 wds:Q59054557-EBEA47CF-979A-45B9-8A1B-A076953456C1 wds:Q59054557-F25C5B40-9C1D-4EF8-AB63-CB378C176FF5 wds:Q59054557-F8E44C81-820E-4DEF-BA76-51D06B4F78CF wds:Q59054557-FEA9728E-0A56-4500-A2BF-EDF548AED164
cites work	Spinel elasticity and seismic structure of the transition zone of the mantle Sharpness of upper-mantle discontinuities determined from high-frequency reflections Absence of an aluminous phase in the upper part of the Earth's lower mantle The system Mg2SiO4-Fe2SiO4at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel The Phase Boundary Between agr- and beta-Mg2SiO4 Determined by in Situ X-ray Observation An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle Seismic evidence for silicate melt atop the 410-km mantle discontinuity The Effect of H2O on the 410-Kilometer Seismic Discontinuity A temperature profile of the mantle transition zone The 410-km-depth discontinuity: A sharpness estimate from near-critical reflections High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent minerals Pressure Dependence of Elastic Wave Velocity for beta-Mg2SiO4 and the Composition of the Earth's Mantle Elasticity of forsterite to 16 GPa and the composition of the upper mantle
author name string	wds:Q59054557-4412F658-FD86-47AC-9E79-2AF0E9AA0817 wds:Q59054557-AE55500C-FB92-49F5-839F-F21167DB6565
author name string	Tetsuo Irifune Maiko Isshiki
rdfs:label	Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (en) Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (nl)
skos:prefLabel	Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (en) Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (nl)
name	Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (en) Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (nl)
title	wds:Q59054557-AA3E3286-E75F-4212-B9BF-7231AAD49353
title	Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity (en)
page(s)	wds:Q59054557-FE5906A2-5967-4773-B12F-1898FD3DAE47
page(s)	702-705
instance of	wds:Q59054557-FB859BED-B37B-49CA-938E-B36968F16145
instance of	scholarly article
published in	wds:Q59054557-4190D196-D44A-4B7F-BA5D-CDCBA52BA915
published in	Nature
issue	wds:Q59054557-6798ED26-1CE7-406B-A254-F01EA14C2A2B
volume	wds:Q59054557-935B1BB0-2020-4112-9FC2-880C0EA4D612
issue	6677
volume	392
DOI	wds:Q59054557-1286FBA7-71E5-4AE9-A5A4-57351E54E5DC
DOI	http://dx.doi.org/10.1038/33663
DOI	10.1038/33663
ADS bibcode	wds:Q59054557-13CF64B7-C68E-4C44-A570-1866894AB8A0
ADS bibcode	1998Natur.392..702I
Dimensions Publication ID	wds:Q59054557-6F9CA53E-E7E4-4554-818B-5CD809A77393
Dimensions Publication ID	1006544011
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q59054557
is cites work of	Phase transformations: Implications for mantle structure Elasticity of Majorite and a Majorite-Pyrope solid solution to high pressure: Implications for the Transition Zone Testing plausible upper-mantle compositions using fine-scale models of the 410-km discontinuity Mineralogy and elasticity of the oceanic upper mantle: Origin of the low-velocity zone The valence state and partitioning of iron in the Earth's lowermost mantle Indoor seismology by probing the Earth's interior by using sound velocity measurements at high pressures and temperatures The effect of H2O on partial melting of garnet peridotite at 3.5 GPa Olivine-wadsleyite transition in the system (Mg,Fe)2SiO4 Topography of the transition zone seismic discontinuities Receiver functions in the western United States, with implications for upper mantle structure and dynamics Computer simulation of the Mg2SiO4 phases with application to the 410 km seismic discontinuity Single-crystal elasticity of ringwoodite to high pressures and high temperatures: implications for 520 km seismic discontinuity Inversion of seismic and geodetic data for the major element chemistry and temperature of the Earth's mantle Elasticity of mantle minerals (experimental studies) Sound velocities of majorite garnet and the composition of the mantle transition region Mantle oxidation state and oxygen fugacity: Constraints on mantle chemistry, structure, and dynamics A mineralogical model for density and elasticity of the Earth's mantle Phase transitions of harzburgite and buckled slab under eastern China Iron speciation in minerals and glasses probed by $$\hbox{M}_{2/3}$$ M 2 / 3 -edge X-ray Raman scattering spectroscopy Temperature dependence of elastic moduli of β-(Mg, Fe)2SiO4 Using the Earth as a polarized electron source to search for long-range spin-spin interactions An experimental study of phase transformations in olivine under pressure and temperature conditions corresponding to the mantle transition zone Comparative compressibility of hydrous wadsleyite and ringwoodite: Effect of H2 O and implications for detecting water in the transition zone Velocity anomalies and spatial distributions of physical properties in horizontally lying slabs beneath the Northwestern Pacific region Elasticity of hydrous wadsleyite to 12 GPa: Implications for Earth's transition zone Olivine emerges from isolation Orthoenstatite/clinoenstatite phase transformation in MgSiO3at high‐pressure and high‐temperature determined by in situ X‐ray diffraction: Implications for nature of the X discontinuity A new high-pressure form of Mg2SiO4 highlighting diffusionless phase transitions of olivine.
is cites work of	wds:Q29014539-D02C19A1-D9A1-4872-BBF2-250B3EA7E648 wds:Q63930525-F494036D-CA9A-4E20-9C1C-3D0CA0C1319D wds:Q59807033-E7D037AB-C470-4363-96DC-C5CCBB1F4A88

Faceted Search & Find service v1.16.117 as of May 05 2024

Alternative Linked Data Documents: ODE Content Formats:

RDF

ODATA

Microdata

About

OpenLink Virtuoso version 07.20.3239 as of May 5 2024, on Linux (x86_64-centos_6-linux-gnu), Single-Server Edition (378 GB total memory, 152 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software