Seismic properties and anisotropy of the continental crust: Predictions based on mineral texture and rock microstructure

BSG Almqvist, D Mainprice - Reviews of Geophysics, 2017 - Wiley Online Library
Progress in seismic methodology and ambitious large‐scale seismic projects are enabling
high‐resolution imaging of the continental crust. The ability to constrain interpretations of …

Faults (shear zones) in the Earth's mantle

A Vauchez, A Tommasi, D Mainprice - Tectonophysics, 2012 - Elsevier
Geodetic data support a short-term continental deformation localized in faults bounding
lithospheric blocks. Whether major “faults” observed at the surface affect the lithospheric …

[BOOK][B] Introduction to the Physics of the Earth's Interior

JP Poirier - 2000 - books.google.com
Enlarged and fully updated, this new edition takes into account the considerable
experimental and theoretical progress recently made in the field. Introduction to the Physics …

The misorientation index: Development of a new method for calculating the strength of lattice-preferred orientation

P Skemer, I Katayama, Z Jiang, S Karato - Tectonophysics, 2005 - Elsevier
Using orientation data from experimentally deformed olivine, we explore some practical
problems with the J-index, a commonly applied measure of fabric strength. We show that the …

Effect of water and stress on the lattice-preferred orientation of olivine

H Jung, I Katayama, Z Jiang, T Hiraga, SI Karato - Tectonophysics, 2006 - Elsevier
The influence of water and stress on the lattice-preferred orientation (LPO) of olivine
aggregates was investigated through large strain, shear deformation experiments at high …

2.16 Seismic anisotropy of the deep Earth from a mineral and rock physics perspective

D Mainprice - Treatise on geophysics, 2010 - books.google.com
In this section the contribution of CPO to seismic anisotropy in the deep Earth with cases of
olivine and the role of melt is illustrated. The CPO in rocks of upper-mantle origin is now well …

Dehydration-driven stress transfer triggers intermediate-depth earthquakes

TP Ferrand, N Hilairet, S Incel, D Deldicque… - Nature …, 2017 - nature.com
Abstract Intermediate-depth earthquakes (30–300 km) have been extensively documented
within subducting oceanic slabs, but their mechanics remains enigmatic. Here we decipher …

Effects of melt depletion on the density and seismic velocity of garnet and spinel lherzolite

DL Schutt, CE Lesher - Journal of Geophysical Research: Solid …, 2006 - Wiley Online Library
We examine the effects of melt depletion on density and anharmonic VP and VS on the
basis of the melting relations of fertile peridotite between 1 and 7 GPa. We incorporate the …

The seismic anisotropy of the Earth's mantle: from single crystal to polycrystal

D Mainprice, G Barruol, WB Ismaïl - … from the atomic scale to the …, 2000 - hal.univ-reunion.fr
The anisotropic single crystal seismic properties are reviewed in the light of recent
experimental and theoretical determinations. Although considerable progress has been …

Fault-induced seismic anisotropy by hydration in subducting oceanic plates

M Faccenda, L Burlini, TV Gerya, D Mainprice - Nature, 2008 - nature.com
The variation of elastic-wave velocities as a function of the direction of propagation through
the Earth's interior is a widely documented phenomenon called seismic anisotropy. The …