爬行洞穴可以在柔性剪切区域建立一个动态的颗粒状流体
F Fusseis1, K Regenauer-Lieb, J Liu
1School of Earth & Environment, The University of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia. fusseis@cyllene.uwa.edu.au
Nature
|June 19, 2009
概括
在地中部剪切区域的流体迁移和岩石变形是相关的. 一个新的模型显示了合变孔隙生成如何驱动流体流动,这对于地震和矿物沉积至关重要.
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
- 地质化学 地质化学
背景情况:
- 在地中部剪切区域的流体迁移和岩石变形之间的相互作用对于地震核形成,俯冲启动和矿石沉积物形成至关重要.
- 经典模型无法解释热,柔性中间地中的流体迁移,其中断裂持续的透性和平衡湿角度不适用.
研究的目的:
- 研究在地中部剪切区域中控制流体迁移和多孔性生成的机制.
- 开发一种由合的机械和化学过程驱动的同形流体迁移的新模型.
主要方法:
- 高分辨率同步龙X射线断层扫描.
- 扫描电子显微镜. 扫描电子显微镜.
- 一个"粒状流体"模型的配方.
主要成果:
- 证据表明,机械和化学潜能控制了综变形孔隙的产生.
- 一个模型展示了通过粘性谷物边界滑动,爬行化,溶解和沉来动态创建透性多孔性.
- 合成变形流体迁移被提出为由生产驱动的自我维持的过程.
结论:
- "粒状流体"模型解释了通过中间地的流体转移.
- 这一过程对于爬行模式中的应变局部化至关重要,影响板块构造学,矿石沉积物形成,地幔脱气和地震核化.
- 这些发现为了解中层地的爬行不稳定性提供了一个关键组成部分.
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