使用地震正常模式的地幔衰减的全球3D模型
Sujania Talavera-Soza1, Laura Cobden2, Ulrich H Faul3,4
1Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands. s.a.talaverasoza@uu.nl.
Nature
|January 22, 2025
概括
这项研究呈现了第一个全的3D地震减弱模型, 它显示了上层地幔的热起源和下层地幔的组成差异,澄清了地幔对流动.
科学领域:
- 地质学
- 地震学
- 地球科学
背景情况:
- 仅仅地震速度模型无法区分地球深层结构的热和组成起源.
- 了解地幔对流需要区分热和组成的影响.
- 全球3D衰减模型以前仅限于上层地幔.
研究的目的:
- 为整个地幔开发一个全面的3D全球衰减模型.
- 使用地震减弱来区分地球3D结构的热和组成起源.
- 增强对地幔对流演变的理解.
主要方法:
- 使用全地球地震振荡构建一个3D全球衰减模型.
- 限制地震减弱到四度的球体波.
- 集成的地震波速度与衰减数据.
主要成果:
- 证实了上层地幔的热源, 高衰减与低速度相关.
- 在地幔下方观察到相反的情况:在地震快速的区域 ("环绕太平洋") 观察到高衰减,在大型低地震速度的省份 (LLSVPs) 观察到低衰减.
- 解释环太平洋地区较冷,粒度较小,与较温暖,较大粒度的LLSVPs形成对比.
结论:
- 新模型提供了对整个地幔异质性和对流的关键见解.
- 根据推断的温度和粒度变化,LLSVPs被证实是长寿命,稳定的特征.
- 这项发现有助于我们更好地了解塑造地球地幔的动态过程.
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