The lithosphere-asthenosphere boundary

KM Fischer, HA Ford, DL Abt… - Annual Review of Earth …, 2010 - annualreviews.org
Seismological models of upper-mantle structure are providing new constraints on the
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …

Seismic tomography: A window into deep Earth

N Rawlinson, S Pozgay, S Fishwick - Physics of the Earth and Planetary …, 2010 - Elsevier
The goal of this paper is to provide an overview of the current state of the art in seismic
tomography, and trace its origins from pioneering work in the early 1970s to its present …

Subduction factory: 4. Depth‐dependent flux of H2O from subducting slabs worldwide

PE Van Keken, BR Hacker… - … Research: Solid Earth, 2011 - Wiley Online Library
A recent global compilation of the thermal structure of subduction zones is used to predict
the metamorphic facies and H2O content of downgoing slabs. Our calculations indicate that …

Grainsize-sensitive viscoelastic relaxation in olivine: Towards a robust laboratory-based model for seismological application

I Jackson, UH Faul - Physics of the Earth and Planetary Interiors, 2010 - Elsevier
Torsional forced oscillation data for a newly prepared specimen of dry, melt-free
polycrystalline Fo90 olivine of 3.1 μm average grainsize have been used to reassess …

Water distribution across the mantle transition zone and its implications for global material circulation

S Karato - Earth and Planetary Science Letters, 2011 - Elsevier
Various methods for inferring the water distribution in Earth's mantle are reviewed including
geochemical and geophysical methods. The geochemical approach using the water …

On the origin of the asthenosphere

S Karato - Earth and Planetary Science Letters, 2012 - Elsevier
Various models of the origin of the asthenosphere are reviewed based on the latest
observations on mineral physics of mechanical properties, melting relationships and the …

Redox-influenced seismic properties of upper-mantle olivine

CJ Cline Ii, UH Faul, EC David, AJ Berry, I Jackson - Nature, 2018 - nature.com
Lateral variations of seismic wave speeds and attenuation (dissipation of strain energy) in
the Earth's upper mantle have the potential to map key characteristics such as temperature …

Mechanisms and geologic significance of the mid-lithosphere discontinuity in the continents

S Karato, T Olugboji, J Park - Nature geoscience, 2015 - nature.com
The stable continents have a puzzling structure. Recent seismological studies have
revealed a marked drop in seismic velocity at middle-lithosphere depths, but a generally …

[PDF][PDF] 1.25—deep earth structure: Q of the Earth from crust to core

B Romanowicz, B Mitchell - Treatise on geophysics, 2015 - scholar.archive.org
Seismic waves have long been known to attenuate at a rate greater than that predicted by
geometric spreading of their wave fronts. Knopoff (1964) pointed out more than four decades …

Site-specific hydrogen diffusion rates in forsterite

JA Padrón-Navarta, J Hermann, HSC O'Neill - Earth and Planetary Science …, 2014 - Elsevier
Synthetic hydroxylated titanium-bearing and undoped MgO-buffered forsterite crystals were
heated at atmospheric pressure in air at temperatures from 800 to 1200° C to determine …