Published March 23, 2022 | Version v1

Low thermal conductivity of hydrous phase D leads to a self-preservation effect within a subducting slab

  • 1. Institute of Earth Sciences, Academia Sinica
  • 2. Bayerisches Geoinstitut, University of Bayreuth
  • 3. Center for High Pressure Science and Technology Advanced Research, Beijing, 100094, China
  • 4. Geodynamics Research Center, Ehime University
  • 5. Department of Earth Science, Graduate School of Science, Tohoku University

Description

This repository contains experimental data on the thermal conductivity of hydrous phase D mineral at high pressure and temperature. This dataset is presented in a manuscript submitted by Wen-Pin Hsieh, Enrico Marzotto, Takayuki Ishii, Leonid Dubrovinsky, Alena A. Aslandukova, Giacomo Criniti, Yi-Chi Tsao, Chun-Hung Lin, Jun Tsuchiya, and Eiji Ohtani entitled:

Low thermal conductivity of hydrous phase D leads to a self-preservation effect within a subducting slab

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