可变的板块动力学促进了沿东北欧亚板块边界沿线的后弧变形模式的变化
Eleonora Ficini1, Marco Cuffaro2, Carlo Doglioni3,4
1CNR-IGAG, Rome, Italy.
Scientific reports
|March 28, 2024
概括
地幔流动显著影响后方弧盆的形成,推动了石灰岩层的延伸. 俯冲沟迁移也起着关键作用,导致这些地质特征的交替压缩和延伸.
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
- 地力学是什么?地力学是什么?
背景情况:
- 由于板块退缩,在弧系统后面形成后方弧盆.
- 对于盆地形成来说,了解覆盖板块的石质层变形至关重要.
研究的目的:
- 为了研究在俯冲过程中覆盖板中的变形模式的演变.
- 探索背弧盆地形成背后的机制,包括东中国海,日本海和库里尔盆地.
主要方法:
- 使用先进的热力学数值模拟.
- 自57万年前以来,太平洋板块的内置动力变异性.
- 包括一个低速度区域在天层和水平地幔流.
主要成果:
- 证明了地幔流在石层延伸和后弧盆地开放中的关键作用.
- 突出了潜水沟位置的动力控制 (前进/后退约100公里).
- 在后弧盆地内确定了压缩和延伸的交替阶段.
结论:
- 地幔流是后弧盆地发展的主要驱动因素.
- 俯冲沟的动力学显著影响变形模式,导致周期性压缩和延伸.
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