This study provides a comprehensive review of the crystal preferred orientation (CPO) of
olivine and orthopyroxene in the upper mantle, and of several hydrous minerals in the …

This study presents the structural and petrological characteristics of mantle peridotites in
relation to the rock-hydrous melt reaction found in the Hayachine ultramafic complex, NE …

Rheology of rocks controls the deformation of the Earth at various space-time scales, which
is crucial to understand the tectonic evolution of continental lithosphere. Researches of rock …

Melt-rock interaction, a general term describing various processes including cryptic and
modal metasomatism and melt-rock reaction, is the main process responsible for modifying …

Abstract In the Herbeira massif, Cabo Ortegal Complex, Spain, a well exposed assemblage
of deformed dunites and pyroxenites offers a unique opportunity to investigate key upper …

To advance our understanding of the deformation characteristics, rheological behaviors, and
tectonic evolution of the fore‐arc lithospheric mantle, we analyzed mineral fabrics for a large …

Mantle xenoliths from the Southern Alps, New Zealand, provide insight into the origin of
mantle seismic anisotropy related to the Australian‐Pacific plate boundary. Most xenoliths …

Understanding lattice-preferred orientations (LPOs) of olivine is important in the study of
seismic anisotropy and mantle flow of the upper mantle in the earth. Although olivine is the …

The large‐volume lithospheric mantle xenoliths around the Dama** area provides
valuable insights into the detailed destruction progression of the North China Craton (NCC) …

Abstract Comparison between geophysical observations and laboratory measurements
yields contradicting estimations of the melt fraction for the partially molten regions of the …