在背弧被动边缘设置中,地幔上游的表面表达的地约束
Jeong-Yeon Hwang1, Sung-Joon Chang2,3, Yu Jin Sohn4
1Interdisciplinary Program in Earth Environment System Science and Engineering, Kangwon National University, Chuncheon, South Korea.
Scientific reports
|November 1, 2025
概括
被动边缘揭示了地幔上升如何影响地形. 韩国甘省的地特性调节了这些热效应,影响了表面的高度和山脉.
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
- 地震学 地震学
背景情况:
- 由于静止,被动边缘保留了构造学和地形学信号.
- 韩国的甘省,由东海背弧开口形成,是一个关键的研究领域.
- 了解地对地幔上升的影响对于被动边缘动态至关重要.
研究的目的:
- 在被动边缘设置中研究地幔上升,地结构和表面升高之间的关系.
- 分析地震速度和Vp/Vs比率以推断热条件和地组成.
- 为了建模影响地幔动态的地形表达的地性质.
主要方法:
- 远震接收器功能的联合反转和雷利波分散数据.
- 对Vp/Vs比率和残余地形的分析.
- 高分辨率的S波地速度建模.
主要成果:
- 在沿海地区下方的地中检测到低S波速度和高Vp/Vs比率,表明浅地幔热效应.
- 在泰贝克山脉以西,低速度仅限于较低Vp/Vs比率的下层地.
- 山脉以西的厚厚的状地阻碍了地幔上升的上升热传播.
结论:
- 地的特性显著调节地幔上升的表面和热表达.
- 边缘驱动的对流可能在这种被动边缘设置中驱动地幔上游.
- 这项研究强调了地结构在塑造地形和被动边缘的热体制中的作用.
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