日本地球惑星科学連合2015年大会

講演情報

口頭発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG59] 地球惑星科学におけるレオロジーと破壊・摩擦の物理

2015年5月27日(水) 16:15 〜 18:00 106 (1F)

コンビーナ:*桑野 修(独立行政法人海洋研究開発機構)、大内 智博(愛媛大学地球深部ダイナミクス研究センター)、清水 以知子(東京大学大学院理学系研究科地球惑星科学専攻)、石橋 秀巳(静岡大学大学院理学研究科地球科学専攻)、座長:清水 以知子(東京大学大学院理学系研究科地球惑星科学専攻)

17:48 〜 17:51

[SCG59-P07] かんらん石-輝石多結晶体における鉱物混合層の形成と歪み弱化

ポスター講演3分口頭発表枠

*田阪 美樹1Mark Zimmerman1David Kohlstedt1 (1.ミネソタ大学)

The formation of well-mixed, fine-grained, poly-phase rocks may lead to strain localization and play a key role in the development of the lithosphere asthenosphere boundary (LAB). To understand the mixing process in the olivine + orthopyroxene rocks, we have conducted torsion experiments on samples of iron-rich olivine + orthopyroxene aggregates at a temperature of 1200℃ and a pressure of 300MPa. We fabricated the samples with grain sizes significantly larger than the steady state grain size. The samples were deformed to total shear strains up to γ = 17. We conducted two series of torsion experiments, the first at fixed strain rate to different strains and the second at different strain rates to the same strain.
The stress exponent of n ≈ 3 and grain size exponent of p ≈ 1 were determined from a least-squares fit to the strain rate, stress and grain size data using a power-law creep equation; these values of n and p indicate that our samples deformed by dislocation-accommodated grain boundary sliding. Dynamic recrystallization occurred with significant grain size reduction of both phases in deformed samples. Well-mixed microstructures develop in samples deformed to higher strains at faster strain rates, whereas elongated olivine and pyroxene grains without a mixed texture are observed at lower strain and strain rate. Mixing of the olivine and orthopyroxene phases occurs due to a contribution of interface-reaction-limited diffusion (IRLD) creep [Sundberg and Cooper, 2008]. This IRDL creep process involves diffusion of metal oxides along phase boundaries oriented perpendicular to σ1 to boundaries parallel to σ1 resulting in the formation of new pyroxene grains along boundaries perpendicular to σ1 and olivine grains along boundaries parallel to σ1. Grain size reduction due to dynamic recrystallization of olivine and orthopyroxene enhance the rate of this process.