Textural evolution during high-pressure dehydration of serpentinite to peridotite and its relation to stress orientations and kinematics of subducting slabs: Insights from the Almirez ultramafic massif
Keywords: Subduction zones; Antigorite serpentinite; Chlorite harzburgite; Almirez massif; Microstructures; Stress; Fluid flow; X-raymicro-computed tomography (μ-CT); Electron backscatter diffraction (EBSD); Shape Preferred Orientation (SPO); Crystal Preferred Ori