概括
上层地幔中的水可以产生含水的间歇性酸盐岩. 这种在特定深度的岩形成解释了地震低速区,提供了一个比以前的理论更强大的假设.
科学领域:
- 地质物理学和地质化学
- 石化学 石化学是一门学科.
- 地震学 地震学
背景情况:
- 上层地幔的地震低速区是理解地球结构的关键特征.
- 以前对低速度区域的解释缺乏全面的支持证据.
研究的目的:
- 为了研究水在上层地幔中的作用.
- 为地震低速区的起源提供新的解释.
主要方法:
- 对于gabbro-水和peridotite-水系统的实验阶段图分析.
主要成果:
- 实验数据表明,上层地幔中存在水的存在导致水性间歇性酸盐岩的产生.
- 岩生成发生在与低速度区域开始一致的深度.
结论:
- 由于上层地幔中存在水的间歇性酸盐岩存在,为地震低速度区域提供了令人信服的解释.
- 这种假设比现有的低速度区域模型更令人满意.
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