scholarly article | Q13442814 |
P6179 | Dimensions Publication ID | 1019278063 |
P356 | DOI | 10.1038/35087500 |
P698 | PubMed publication ID | 11484043 |
P5875 | ResearchGate publication ID | 11859152 |
P50 | author | George R. Helffrich | Q57884451 |
P2093 | author name string | Wood BJ | |
P2860 | cites work | A detailed map of the 660-kilometer discontinuity beneath the izu-bonin subduction zone | Q80916487 |
Thermal evolution models for the Earth | Q87751226 | ||
Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust | Q97322585 | ||
Speculations on the Consequences and Causes of Plate Motions | Q98013045 | ||
Gradual entrainment of a chemical layer at the base of the mantle by overlying convection | Q107112977 | ||
Phase transformations and their bearing on the constitution and dynamics of the mantle | Q107275057 | ||
Phase transformations and partitioning relations in peridotite under lower mantle conditions | Q107275311 | ||
Thermoelastic properties and crystal structure of MgSiO3 perovskite at lower mantle pressure and temperature conditions | Q107275368 | ||
Seismic evidence against a mantle chemical discontinuity near 660 km depth beneath Izu-Bonin | Q107275426 | ||
Topography of the 660-km seismic discontinuity beneath Izu-Bonin: Implications for tectonic history and slab deformation | Q107275439 | ||
Density and composition of the lower mantle | Q107275627 | ||
Heat flow from the Earth's interior: Analysis of the global data set | Q22122451 | ||
The composition of the Earth | Q29396953 | ||
Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications | Q30040418 | ||
Compositional stratification in the deep mantle | Q41614410 | ||
Dipping low-velocity layer in the mid-lower mantle: evidence for geochemical heterogeneity | Q47725090 | ||
Thermoelasticity of Silicate Perovskite and Magnesiowustite and Stratification of the Earth's Mantle. | Q52415929 | ||
The age of the Earth | Q55871893 | ||
The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system | Q56049107 | ||
Mantle geochemistry: the message from oceanic volcanism | Q56136782 | ||
Phase transition Clapeyron slopes and transition zone seismic discontinuity topography | Q56680247 | ||
In search of a bulk-Earth composition | Q57382602 | ||
Making continental crust | Q58156625 | ||
Rutile-Bearing Refractory Eclogites: Missing Link Between Continents and Depleted Mantle | Q58760997 | ||
Evidence for partial melt at the core–mantle boundary north of Tonga from the strong scattering of seismic waves | Q58989480 | ||
Implications of a two-component marble-cake mantle | Q59052513 | ||
Iceland Mantle Plume: Geochemical Study of Reykjanes Ridge | Q59055332 | ||
Transition region of the Earth's upper mantle | Q59056516 | ||
K, U and Th in mid-ocean ridge basalt glasses and heat production, K/U and K/Rb in the mantle | Q59057033 | ||
The post-spinel phase of forsterite | Q59079295 | ||
Heat and helium in the Earth | Q59080122 | ||
Earth's neodymium budget and structure and evolution of the mantle | Q59080320 | ||
The core–mantle boundary layer and deep Earth dynamics | Q59091706 | ||
Seismic evidence for small-scale heterogeneity throughout the Earth's mantle | Q59092345 | ||
Upper-mantle seismic discontinuities and the thermal structure of subduction zones | Q59092566 | ||
Tomographic imaging of subducted lithosphere below northwest Pacific island arcs | Q59098742 | ||
An experimental study of subduction and slab migration | Q59409470 | ||
Global mapping of topography on transition zone velocity discontinuities by stackingSSprecursors | Q59857989 | ||
Small scatterers in the lower mantle observed at German broadband arrays | Q60708483 | ||
The chemical composition of subducting sediment and its consequences for the crust and mantle | Q62089302 | ||
Constraints on seismic velocities in the Earth from traveltimes | Q63344509 | ||
Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness | Q64384903 | ||
P433 | issue | 6846 | |
P407 | language of work or name | English | Q1860 |
P304 | page(s) | 501-507 | |
P577 | publication date | 2001-08-01 | |
P1433 | published in | Nature | Q180445 |
P1476 | title | The Earth's mantle | |
P478 | volume | 412 |
Q107269110 | A Sequence of up to 11 Seismic Discontinuities Down to the Midmantle Beneath Southeast Asia |
Q60722467 | Absence of density crossover between basalt and peridotite in the cold slabs passing through 660 km discontinuity |
Q107269113 | Application of Ps Scattering Kernels to Imaging the Mantle Transition Zone With Receiver Functions |
Q60714809 | CaSiO3 perovskite at lower mantle pressures |
Q98749172 | Comparison of Magnitude Estimates for New Zealand Earthquakes: Moment Magnitude, Local Magnitude, and Teleseismic Body-Wave Magnitude |
Q64387126 | Computational support for a pyrolitic lower mantle containing ferric iron |
Q57786794 | Do We Really Need Mantle Components to Define Mantle Composition? |
Q42037879 | Fractionation of elements by particle size of ashes ejected from Copahue Volcano, Argentina. |
Q107269093 | Global slab deformation and centroid moment tensor constraints on viscosity |
Q59068717 | Helium isotopic evidence for episodic mantle melting and crustal growth |
Q53641747 | In silico infrared and Raman spectroscopy under pressure: the case of CaSnO3 perovskite. |
Q107271026 | Inversion of seismic and geodetic data for the major element chemistry and temperature of the Earth's mantle |
Q27350558 | Joint diffraction and modeling approach to the structure of liquid alumina |
Q51318539 | Lamination and mixing in three fundamental flow sequences driven by electromagnetic body forces. |
Q105594401 | Lower-mantle water reservoir implied by the extreme stability of a hydrous aluminosilicate |
Q107269112 | Mantle Transition Zone Thickness Beneath the Middle East: Evidence for Segmented Tethyan Slabs, Delaminated Lithosphere, and Lower Mantle Upwelling |
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Q107269089 | On mantle chemical and thermal heterogeneities and anisotropy as mapped by inversion of global surface wave data |
Q107269095 | On the heterogeneous electrical conductivity structure of the Earth’s mantle with implications for transition zone water content |
Q107271089 | Origin of ocean island basalts: A new perspective from petrology, geochemistry, and mineral physics considerations |
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