缓慢的热化学基底地幔结构支持它们的长寿稳定性
Zhidong Shi1,2, Ross N Mitchell1,2, Yang Li3,4
1State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.
Nature communications
|November 20, 2024
概括
数字模型显示,深层地幔中的大型低剪波速度省 (LLSVPs) 可能是由热化学结构形成的. 这些古老的,缓慢移动的特征解释了几百万年的地质观测.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 地幔动力学地幔动力学
背景情况:
- 大型低剪波速度省 (LLSVPs) 是地球深层地幔中神秘的大型结构.
- 地质证据表明,LLSVPs至少已经稳定了2亿年.
研究的目的:
- 调查LLSVP的起源和长期稳定性.
- 模拟基底地幔结构的形成,类似于LLSVP.
主要方法:
- 覆盖层对流的数值建模,包括板状的行为.
- 模型的参数化以匹配观察到的LLSVP特征.
主要成果:
- 一个类似太平洋的下流腰带成功地产生了两个与LLSVP类似的反足基底地幔结构.
- 模拟的热化学结构表现出速度比环境地幔慢大约四倍,与长期稳定性一致.
结论:
- 模拟的基本地幔结构的缓慢,热化学性质支持它们的古老起源和稳定性.
- 这提供了一个潜在的机制,将几亿年的地质观测与现代的LLSVPs联系起来.
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