Abstract. The texture development in experimentally sheared aggregates of olivine was monitored as a function of increased water content and added melt. In dry samples, an alignment of {010} with the shear plane and <100> and <001> with the shear direction, respectively, was observed, consistent with intracrystalline glide on the (010) [100] an
Observation and analysis of seismic waves is the predominant mechanism in which geophysicists i...
As a major mantle mineral with volume fraction >60%, olivine is assumed to control the rheology of t...
International audienceSeveral thermally activated mechanisms have been proposed to explain the dynam...
International audienceWe performed torsional deformation experiments on pre-hydrated fine-grained ol...
I will deform natural olivine aggregates (Anita Bay dunite) cores in various orientations relative t...
AbstractThe development of crystallographic textures in olivine-rich rocks leads to a marked anisotr...
The development of crystallographic textures in olivine-rich rocks leads to a marked anisotropy in v...
The Earth\u27s upper mantle, mainly composed of olivine, is seismically anisotropic. Seismic anisotr...
Convecting mantle plays a central role in the thermal and geochemical evolution of the Earth. It pro...
A marked anisotropy in viscosity develops in Earth's mantle as deformation strongly aligns the cryst...
International audiencePolycrystalline samples of San Carlos olivine were deformed at high-pressure (...
Publisher's PDFThe significant viscous anisotropy that results from crystallographic alignment (text...
The Lindas Nappe, Bergen Arc, is located in western Norway and displays two high-grade metamorphic s...
The nature of lattice‐preferred orientation (LPO) in olivine‐rich rocks strongly influences many imp...
International audienceTo better constrain the rheology of the mantle, experimental studies on olivin...
Observation and analysis of seismic waves is the predominant mechanism in which geophysicists i...
As a major mantle mineral with volume fraction >60%, olivine is assumed to control the rheology of t...
International audienceSeveral thermally activated mechanisms have been proposed to explain the dynam...
International audienceWe performed torsional deformation experiments on pre-hydrated fine-grained ol...
I will deform natural olivine aggregates (Anita Bay dunite) cores in various orientations relative t...
AbstractThe development of crystallographic textures in olivine-rich rocks leads to a marked anisotr...
The development of crystallographic textures in olivine-rich rocks leads to a marked anisotropy in v...
The Earth\u27s upper mantle, mainly composed of olivine, is seismically anisotropic. Seismic anisotr...
Convecting mantle plays a central role in the thermal and geochemical evolution of the Earth. It pro...
A marked anisotropy in viscosity develops in Earth's mantle as deformation strongly aligns the cryst...
International audiencePolycrystalline samples of San Carlos olivine were deformed at high-pressure (...
Publisher's PDFThe significant viscous anisotropy that results from crystallographic alignment (text...
The Lindas Nappe, Bergen Arc, is located in western Norway and displays two high-grade metamorphic s...
The nature of lattice‐preferred orientation (LPO) in olivine‐rich rocks strongly influences many imp...
International audienceTo better constrain the rheology of the mantle, experimental studies on olivin...
Observation and analysis of seismic waves is the predominant mechanism in which geophysicists i...
As a major mantle mineral with volume fraction >60%, olivine is assumed to control the rheology of t...
International audienceSeveral thermally activated mechanisms have been proposed to explain the dynam...