Thermal diffusivity of forsterite at high pressures and high temperatures

スポンサーリンク

概要

• 論文の詳細を見る

• Thermal diffusivity of synthetic forsterite was measured in the temperature range from 350 to 1500 K at 0 and 6 GPa. Reciprocal thermal diffusivity cannot be regarded as a linear function of absolute temperature. Thermal diffusivity of forsterite increases by ca. 40% over 6 GPa.

• 日本鉱物科学会の論文
• 2002-10-01

著者

• KATSURA Tomoo

  Institute for Study of the Earth's Interior, Okayama University

• Katsura Tomoo

  Institute For Study Of The Earth's Interior Okayama University

関連論文

• Electrical conductivity measurements of brucite under crustal pressure and temperature conditions
• Detailed Structures of Hexagonal Diamond (Ionsdaleite) and Wurtzite-type BN
• Thermal diffusivity of forsterite at high pressures and high temperatures
• The temperature-pressure-volume equation of state of γ-Mg_2SiO_4
• Detailed Structures of Hexagonal Diamond (lonsdaleite) and Wurtzite-type BN
• Crystal structure of anhydrous phase X, K_(Mg_Cr_)Si_O_7
• Crystal structure of anhydrous phase X, K1.93(Mg2.02Cr0.02)Si2.00O7
• Stability of Magnesite under the Lower Mantle Conditions.

スポンサーリンク