在部分化聚合物中化和剪切局部化的动态
Richard F Katz1, Marc Spiegelman, Benjamin Holtzman
1Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA. katz@ldeo.columbia.edu
Nature
|August 11, 2006
概括
在中海山脊下聚焦的岩是由新的理论模型解释的. 这些模型揭示了如何在特定的角度形成融化带,增强岩流向山脊轴.
科学领域:
- 地质物理学 地质物理学
- 地幔动态地幔动态
- 火山学 火山学是一门学科.
背景情况:
- 火山由地幔融化养,但其聚焦机制尚不清楚.
- 融化提取和聚焦是构造界限上的关键过程.
- 中洋山脊是理解地幔融化动态的关键地点.
研究的目的:
- 为了研究中海山脊下面的融化聚焦机制.
- 为了解释在实验中观察到的高孔度融化带的形成.
- 为了使理论预测与带角度的实验观测相协调.
主要方法:
- 开发了一种新的理论公式,用于岩动力学.
- 模拟实验室实验融聚焦的模型.
- 分析了孔隙性减弱和应变率减弱机制之间的平衡.
主要成果:
- 确定化带在与剪切平面相比15-25度处形成.
- 通过对变形机制的平衡来解释观察到的带角.
- 证明,延展率的增强减弱导致带角较低.
结论:
- 新模型准确地解释了实验融化带的形成.
- 可以估计在中洋山脊下面的融化带方向.
- 增强的岩聚焦到山脊轴是可能的后果.
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