[S-CG55] Oceanic plate as inputs to subduction zone and the subduction initiation

[SCG55-P06] In-situ deformation of antigorite-olivine two-phase mixtures: implications for dynamics and seismic anisotropy in the mantle wedge

Hurlow Roselyn^2,3, Wenhao Su¹, Wen-Yi Zhou¹, Feng Lin⁴, Lowell Miyagi⁴, Timothy Officer⁵, Tony Yu⁵, Yanbin Wang⁵, Meiqian Wu⁶, Qin Wang⁶, *Jin Zhang¹ (1. Texas A&M University College Station, 2. Lawrence Livermore National Laboratory, 3. University of New Mexico, 4. University of Utah, 5. The University of Chicago, 6. Nanjing University)

Keywords:crystallographic preferred orientation, seismic anisotropy, two phase mixture, mantle wedge