地幔超塑性及其自制死亡
Takehiko Hiraga1, Tomonori Miyazaki, Miki Tasaka
1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan. hiraga@eri.u-tokyo.ac.jp
Nature
|December 24, 2010
概括
地质材料表现出超可塑性,在没有故障的情况下变形超过500%. 这种地幔岩石的行为涉及谷物边界滑动和显著的谷物生长,影响地幔粘度.
科学领域:
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
- 矿物物理 矿物物理
背景情况:
- 超塑性,即固体材料经历巨大的塑性变形的能力,在金属和陶方面得到了充分证实.
- 它的存在在地质材料中,如冰盖和地球地幔,长期以来一直被推测,但在实验中未得到证实.
研究的目的:
- 通过实验证明和描述与地球地幔相关的地质材料中的超塑性.
- 为了研究这些类似物中超塑性流动期间的变形机制和相关的微观结构演变.
主要方法:
- 在亚固体条件下,对多晶石+危险 (9:1) 和石+静态石+二氧化 (7:2.5:0.5) 类似物进行实验变形.
- 分析微观结构变化,包括粒度变化和变形机制 (粒度边界滑动).
主要成果:
- 地质材料类似物无故障实现了高达500%的均质延长,证实了超塑性.
- 变形伴随着应变硬化,归因于通过谷物边界滑动的谷物生长.
- 建立了一个经验性的菌株-颗粒大小-粘度关系.
结论:
- 地球地幔中的超塑性流,特别是在剪切区和潜伏板块中,是合理的.
- 地幔超塑性不可避免地导致显著的谷物生长,增加粘度,并最终停止流动.
- 这种微观结构的进化影响了地幔动力学和质学.
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