深地幔地震与中大西洋山脊的CO2脱气有关
Zhiteng Yu1,2,3, Satish C Singh4, Cédric Hamelin5
1Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China. ztyu@sio.org.cn.
Nature communications
|January 10, 2025
概括
沿中大西洋山脊的深地幔地震与二氧化碳 (CO2) 与原始融物脱气有关. 这种二氧化碳的释放影响了石化层-石化层边界以下的融化存在.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 石化学 石化学是一门学科.
背景情况:
- 像二氧化碳 (CO2) 和水 (H2O) 这样的挥发物对海洋扩散中心的地幔融化至关重要.
- 这些挥发性物质在地幔融化迁移过程中的作用尚不清楚.
研究的目的:
- 为了调查深地幔地震的原因,沿着中大西洋山脊沿着脆软的边界下方.
- 了解富含挥发性物质的融对地幔过程的影响.
主要方法:
- 分析来自海底地震仪的地震学数据,以检测深度地震.
- 对区域基岩岩样本进行地质化学分析,以确定融化的组成.
主要成果:
- 在中大西洋山脊轴下面的地幔中,在10-20公里深处检测到深度地震.
- 岩岩样本显示,初级融物中的二氧化碳度异常高 (0.4-3.0 wt%).
- 这些融物中溶解的二氧化碳的脱气导致体积变化,可能引发深度地震.
结论:
- 这个地区的深层地幔地震归因于原始化的二氧化碳脱气.
- 原始融中的高二氧化碳度显著影响了融在石化层-石化层边界的存在,温度低于固体.
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