由压力扰动引起的地球深层加快水合
B Jamtveit1, H Austrheim, A Malthe-Sørenssen
1Department of Geology, University of Oslo, Norway. bjorn.jamtveit@geologi.uio.no
Nature
|November 18, 2000
概括
外部液体对于地球干燥的下层地的逆向变形是必不可少的. 由流体岩石反应引起的应力场变化加速了流体运输到岩石中,影响了地的特性.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
背景情况:
- 山脉带形成一个较低的地,最小的自由液体.
- 逆向变形需要外部流体进入干燥的地体积.
- 变态显著改变地的物理性质,如密度和质.
研究的目的:
- 研究流体运输到干燥地岩中的机制.
- 了解流体岩石相互作用如何影响质量运输.
- 分析应力场扰动在流体迁移中的作用.
主要方法:
- 现场观测流体岩石相互作用的变态状态.
- 开发和应用流体运输模拟网络模型.
- 在不同压力条件下分析反应前线形态.
主要成果:
- 流体运输到干岩中是由反应引起的应力场扰动加速的.
- 反应前线形态取决于外部应力场的异构性.
- 大众运输距离超过了简单的谷物边界扩散所预测的距离.
结论:
- 流体-岩石反应积极增强流体透到地.
- 构造压力和流体诱导的压力变化是变形的关键驱动因素.
- 了解这些过程对于解释地的演变和特性至关重要.
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