相关实验视频
Updated: Jun 22, 2026

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Mechanoluminescent Visualization of Crack Propagation for Joint Evaluation
Published on: January 6, 2023
停滞不前的板块的撕裂
Masayuki Obayashi1, Junko Yoshimitsu, Yoshio Fukao
1Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan. obayashi@jamstec.go.jp
概括
日本下面的浮动构造板在它们的交汇处被撕裂. 这种持续的板块撕裂发生在板块在660公里的不连续性上曲和平整时.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 西太平洋的浮沉板块,如伊祖-博宁和日本板块,经常停滞在地幔过渡区.
- 这些停滞板块的机械性能尚不清楚.
- 这两个特定的板块在日本西南部下面形成了一个独特的结合点.
研究的目的:
- 为了研究伊祖-邦宁和日本板块在它们的交汇处的机械行为.
- 为了确定板块是否由于几何约束而遭受撕裂.
- 为正在进行的板块撕裂过程提供证据.
主要方法:
- 板块曲和平整的几何分析.
- 展示了三种不同的证据支持板块撕裂.
- 对地震数据的分析 (隐含).
主要成果:
- 伊祖博宁石板和日本石板在它们的交汇处明显被撕裂.
- 板块撕裂是660公里不连续性的曲和平整的结果.
- 有证据支持正在进行的,活跃的撕裂过程.
结论:
- 沉降的海洋石质层可以在深处经历显著的撕裂.
- 几何因素在引板的变形中起着至关重要的作用.
- 这些发现为地幔过渡区过程的动态提供了新的见解.
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