在地球核心-地幔边界中识别脱水引起的剪切速度异常
Songsong Han1,2,3, Xiaoming Cui1, Baolong Zhang1
1State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China.
Innovation (Cambridge (Mass.))
|January 28, 2025
概括
中美洲下面的深地幔地震异常是由水性阶段H解释的. 在地球深处的水循环可能会导致在D"层深度的剪切波速度增加.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地震学 地震学
背景情况:
- 由于温度梯度,D"层表现出剪切波速度和深度之间的负相关性.
- 在中美洲下方的D"层中观察到与深度的剪切波速度异常增加,这与沉没的法拉隆板块有关.
- 在深层地幔中这种地震速度异常的原因仍然不太清楚.
研究的目的:
- 为了研究中美洲下方D"层的地震速度异常.
- 确定含水矿物质,特别是H相在解释深地幔地震观测中的作用.
- 为了限制水含量和分布对弹性波速的影响.
主要方法:
- 计算水性 H 阶段的热弹性常数,其含量和阴离子配置不同.
- 在相关地幔条件下,确定水性相H的弹性波速.
- 由于脱水和在D"层内的再分配而导致的地震速度变化的建模.
主要成果:
- 水相H表现出明显较低的剪切波速度与后矿类型桥矿相比.
- 富含Al的H相脱水和再分配到干酸盐导致剪切波速度随着深度的逐渐增加.
- 大约3.5%的H相水量足以解释中美洲下方观察到的地震异常.
结论:
- 中美洲下方D"层的地震速度异常可以归因于水性H相的存在和脱水.
- 在该地区观察到的正速度-深度梯度表明深水回收.
- 水性矿物质在地球最底层地幔深处调节地震特性方面发挥着至关重要的作用.
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