基本地幔结构通过超大陆再生
Peng Peng1,2, Ross N Mitchell3,4, Nan Zhang5
1China-South America Joint Research Center, State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China. pengpengwj@mail.iggcas.ac.cn.
Nature communications
|November 3, 2025
概括
连接到地幔羽毛的大火性区域 (LIPs) 表明,在罗丁亚超大陆期间存在着古代的大低剪波速度区域 (LLSVPs). 这些结构显示出超大陆周期之间再生和迁移的迹象.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 板块构造学是一种板块构造学.
背景情况:
- 地球地幔中的大型低剪波速度区域 (LLSVPs) 与超大陆解体期间的大火性区域 (LIPs) 有关.
- 在早期的超级大陆 (如罗丁尼亚) 中,像LLSVPs这样的地幔结构的存在和行为在很大程度上是未知的.
研究的目的:
- 在罗丁亚超大陆期间调查基底地幔结构的存在和特征.
- 分析罗丁亚历史上LIP和潜在LLSVP活动之间的关系.
主要方法:
- 来自中国和巴西的地质样本的分析.
- 整合关于LIPs的现有文献数据.
- 古地理和地幔羽毛活动的多代理重建.
主要成果:
- 鉴定了七个与罗丁亚超大陆 (9400-7200万年前) 相关的LIP.
- 重建揭示了一个LIPs的环,表明一个古老的LLSVP与advecting羽毛.
- Nd同位素数据表明海洋石化层的回收和不断变化的LIP来源.
结论:
- 证据支持在罗丁亚超大陆期间存在一个古老的LLSVP,影响了LIP形成.
- 在超大陆周期之间,LLSVPs表现出再生,补充和迁移的模式.
- 这项研究突出了罗迪尼亚和潘盖亚 LLSVP 活动之间的羽毛向导和古地理学的相似性和差异.
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