在夏威夷火山的演化过程中,地和地幔的融化储存
Esteban Gazel1, Kyle Dayton1, Wenwei Liang1
1Department of Earth and Atmospheric Sciences, Cornell University, 2160 Snee Hall, 112 Hollister Drive, Ithaca, NY 14850, USA.
Science advances
|May 14, 2025
概括
随着太平洋板块的移动,夏威夷火山显示了岩储存深度的变化. 早期的盾牌阶段具有浅层的岩,而后期的阶段涉及更深层的地和地幔储存.
科学领域:
- 地质地质地质地质地质地
- 火山学 火山学是一门学科.
- 地质化学 地质化学
背景情况:
- 太平洋板块在夏威夷地幔羽毛上的迁移影响了岩流,喷发风格和组成.
- 据假设,在从盾牌到后盾和复原阶段的过渡期间,岩储存会变得更深入,变得更短暂.
研究的目的:
- 在夏威夷的不同火山阶段量化调查岩储存深度的演变.
- 为了测试更深,更短暂的融化储存与下降的岩流的假设.
主要方法:
- 使用拉曼光谱法对火山样本进行了高精度的液体包容度计.
- 分析来自不同进化阶段 (盾牌,后盾,再生) 的代表性火山的样本.
主要成果:
- 盾阶段的岩储存 (Kīlauea) 浅,大约为1-2公里.
- 后盾阶段的岩储存 (Haleakalā) 涉及地 (大约. 2公里) 和更深的莫霍水平储存 (20-27公里).
- 复苏阶段的岩储存 (钻石头) 是地幔主导的 (22-30公里).
结论:
- 夏威夷的火山活动显示了岩储存深度的明显演变,与融化流量减少有关.
- 浅层岩储存与盾牌火山中的高流相关.
- 莫霍河成为融化停滞和演变的关键边界,因为在较晚的火山阶段,融化流量减少.
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