来自古代构造的基岩小安提勒斯板块的地震成像
Xusong Yang1,2,3,4, Yujiang Xie3,5, Catherine A Rychert6,7
1State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.
Nature
|April 9, 2025
概括
在地幔深处可以携带化学异常, 这些异常影响了板块的沉降深度,
科学领域:
- 地质学
- 地质化学
- 构造学
背景情况:
- 石化物沉入地幔过渡区 (MTZ).
- 影响板块流动的因素,如化学异质性,尚不清楚.
- 之前的研究已经面临限制地幔流动及其影响因素的挑战.
研究的目的:
- 在小安提利斯海域下面的沉降板块和MTZ的图像.
- 为了研究控制石化层沉降的因素.
- 了解化学异质在地幔动态中的作用.
主要方法:
- 使用P-to-S接收器功能来图像地震断裂.
- 采用了综合地力学和波形建模.
- 分析地震数据以确定深层地幔结构.
主要成果:
- 拍摄了一个超深的 (>700公里) 660公里不连续的潜水板.
- 观察到附近的正常和超深的双重660断裂阶段.
- 地动力学和波形建模显示出一个巨大的基岩丰富的化学异常, 不仅仅是温度的影响.
结论:
- 观测到的地震特征表明岩板中存在大量的化学异常.
- 这种异常很可能与缩的灭绝蔓延山脊有关.
- 过去的构造事件产生了化学异质,影响了板块沉没行为和地幔流动.
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