在加拿大东南部山脉下面的双层地幔石化层
Songyun Huang1, Yu Jeffrey Gu2, Stephen Thomas Johnston3
1Department of Physics, University of Alberta, Edmonton, AB, Canada.
Nature communications
|November 25, 2025
概括
这项研究揭示了加拿大西南部下面的双石层结构,古老的北美克拉顿是 Kordilleran 石层的基础. 西向浸泡的界面表明一个复杂的坑边缘受到地质过程的影响.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地球科学 地球科学 地球科学
背景情况:
- 在加拿大西南部的北美巨的边缘是一个岩层阶段,从 Cordillera 过渡到一个强大的巨.
- 以前的描述缺乏对这个边界区域的详细结构洞察.
研究的目的:
- 用地震方法对加拿大西南部下方的石质层过渡区进行成像.
- 为了研究地边缘的地下结构和架构.
主要方法:
- 利用了对边界区域敏感的转换剪切波.
- 分析了地震数据,以确定向西俯冲的接口和水平剪切速度梯度.
主要成果:
- 在落基山沟 (RMT) 西部发现了向西俯冲的接口.
- 相关的地震界面与水平剪切速度梯度在75公里和180公里深处.
- 揭示了双石层结构与前坎布里亚克拉顿核心下方的 Cordilleran 石层.
结论:
- 克拉顿边缘呈现双石层结构,这表明前坎布里亚克拉顿是 Cordilleran 石层的基础.
- 克拉顿边缘的形态表明过去6000万年来升起和对流侵蚀的影响.
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