数字建模深层板块脱水和岩石化过程
Hao Wu1, Jiacheng Lei1, Zeyu Jia1
1College of Transportation Engineering of Nanjing Tech, Nanjing Tech University, Nanjing, 211816, China.
Scientific reports
|November 4, 2024
概括
沉降区的深层板块脱水导致地幔融化和岩活动. 水运输到深层地幔的影响融化生成和大陆下面的岩腔形成.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
背景情况:
- 海洋和大陆的浮沉区是理解板块动态和岩石运动的关键地质设置.
- 深层板块的水化和脱水过程显著影响地幔地质化学和融化.
- 以前的模型没有完全捕捉到水运输的时间演变及其对深层地幔融化的影响.
研究的目的:
- 通过使用高分辨率的热力学模型,研究潜水区深层板块水化和脱水的动态过程.
- 揭示水运输到深层地幔的途径和时间演变.
- 了解板块脱水在引发部分融化和岩活动中的作用.
主要方法:
- 采用了2D高分辨率热力学合数值模型.
- 该模型模拟了板块构造学,流体运输和热过程之间的复杂相互作用.
- 分析重点是水路,脱水反应和在不同深度产生融.
主要成果:
- 板块脱水是深层地幔部分融化和随后的岩活动的关键触发因素.
- 产生的融体积与深度有很大差异,在更深的区域,脱水反应较弱.
- 在深层地幔中,达到适合水性融的压力-温度 (P-T) 条件需要更长的时间.
结论:
- 向深层地幔的水运输在地质学上很重要,影响了岩过程.
- 深度脱水反应在大陆板下形成岩腔中起着至关重要的作用.
- 这项研究提供了关于潜水区水循环和岩的长期演变的见解.
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