Published November 20, 2021 | Version v1

Seismic Anisotropy in the Lower Mantle Transition Zone Induced by Lattice Preferred Orientation of Akimotoite-Dataset

  • 1. Institute for Planetary Materials, Okayama University
  • 2. Japan Synchrotron Radiation Research Institute

Description

The dataset includes the lattice preferred orientation data of akimotoite aggregates obtained through EBSD and transmitted two-dimensional (2D) X-ray diffraction method at BL04B1 of synchrotron facility of SPring-8, Hyogo, Japan. The employed conditions of 2D X-ray diffraction measurements are also available.

Files

Datasets for LPO of akimotoite.zip

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