活跃板块边界断层的极端热水条件
Rupert Sutherland1,2, John Townend2, Virginia Toy3
1GNS Science, PO Box 30368, Lower Hutt, New Zealand.
Nature
|May 18, 2017
概括
活跃的板块边界断层表现出极端的热水条件,高流体压力和地热梯度,由断层的快速移动和景观发展驱动. 这些条件影响了地震的分布和断层行为.
科学领域:
- 地质学
- 结构地质学
- 构造学
背景情况:
- 温度和流体压力是岩石变形,矿化和地质断层地震分布的关键因素.
- 大陆板内地通常表现出水位流体压力和~31°C/km的地热梯度.
- 由于石英和地的可塑性,高温 (>300-450°C) 在深度>10-15公里促进无地震爬行,减少地震频率.
研究的目的:
- 调查阿尔卑斯山断层上部的温度和流体压力条件,这是一个主要的板块边界断层.
- 了解影响活跃断层的摩擦机械过程和地震破裂周期的热水条件.
主要方法:
- 在阿尔卑斯山断层的悬挂墙上钻孔893米深.
- 在钻井孔内测量孔液压和温度梯度.
- 分析数据以建模断层滑动,流体流动和景观发展的相互作用.
主要成果:
- 钻井发现孔液压梯度超过了水静态水平的9±1%.
- 在断层的悬挂墙上记录了125±55°C/km的平均地热梯度.
- 这些极端条件归因于断层的快速移动和地形驱动的流体流,集中热量.
结论:
- 活跃的板块边界断层可以在地震带中形成高度异常的流体压力和温度梯度.
- 断层滑动,岩石变化和景观演变之间的积极反推动了这些极端的热水条件.
- 这些条件对断层的机械行为和地震潜力产生重大影响.
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