To obtain a better understanding of melt–rock interactions in the upper mantle,
microstructural and petrological analyses were conducted on deformed mantle peridotites …

To understand the processes involved in phase mixing during deformation and the resulting
changes in rheological behavior, we conducted torsion experiments on samples of iron‐rich …

Differential stress magnitude is a fundamental parameter in the study of geodynamic
processes in the continental lithosphere, and is typically estimated in quartz-and olivine …

The effect of pressure, temperature and composition on the development of crystal preferred
orientations (CPO) and seismic properties of olivine-orthopyroxene aggregates were …

Synthesized polycrystalline enstatite samples were deformed in a Paterson gas‐medium
apparatus at 1200–1300° C, oxygen fugacity buffered at Ni/NiO, and confining pressures of …

Intermediate-depth earthquakes that occur between∼ 60-and 300-km depths in subducted
oceanic slabs often form a double band of seismicity. The upper band of seismicity is …

Although the seismic properties of polycrystalline olivine have been the subject of systematic
and comprehensive study at seismic frequencies, the role of orthopyroxene as the major …

Synthesized polycrystalline samples composed of enstatite and olivine with different
volumetric ratios were deformed in compression under anhydrous conditions in a Paterson …

Constraining the stress related to lithospheric deformation in natural rocks is key to develop
and test a geodynamic model. However, the cautions of extrapolating piezometers that are …

Bone is a dynamic and mechanically active tissue that changes in structure over the human
lifespan. The products of the bone remodeling process have been studied substantially …