在新赫布里德群岛的背弧裂过程中,薄弱的化和地幔快速更换
Karsten M Haase1, Marcel Regelous2, Christoph Beier3
1GeoZentrum Nordbayern, Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), Schlossgarten 5, 91054, Erlangen, Germany. karsten.haase@fau.de.
Nature communications
|July 18, 2024
概括
福图纳河谷是通过福图纳河的.
科学领域:
- 地质地质地质地质地质地
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
背景情况:
- 岛屿弧和背弧构造和岩过程的了解很少.
- 引板组成和地幔流影响了这些过程.
研究的目的:
- 为了分析来自Futuna沟的岩年龄和组成.
- 了解地幔源和板块输入随着时间的推移而发生的演变.
主要方法:
- 分析海底岩的年龄和化学成分.
- 地质化学解释地幔源进化.
主要成果:
- 较古老的岩 (>2.5亿年) 起源于一个具有显著板块元相性质的丰富地幔源.
- 较年轻的岩显示了板块输入量减少到一个枯竭的地幔.
- 在过去的250万年里,地幔的快速替换和板块的化发生了.
结论:
- 地幔的组成和动力学显著影响后方弧形岩.
- 粗的回滚和坡驱动了地幔的快速更换和后弧裂.
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