由地磁信号揭示的东亚中亚矿产带下地幔过渡区的电导率
Yanhui Zhang1,2, Yujia Hu3,4, Mina Ma3,4
1School of Safety Engineering and Emergency Management, Shijiazhuang Tiedao University, Shijiazhuang, 050043, China. global_em@163.com.
Scientific reports
|January 8, 2025
概括
中亚矿产带的火山活动与深层地幔结构有关. 地幔过渡区的高导电异常表明海洋地或分层物质停滞不前,导致岩上升和火山活动.
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
- 火山学 火山学是一门学科.
背景情况:
- 中亚东部黄岩带 (CAOB) 的广泛火山活动缺乏对其形成机制和物质来源的明确解释.
- 地幔过渡区 (MTZ) 在地幔物质和能量转移中起着关键作用,可能限制火山动态.
研究的目的:
- 通过使用地磁深度探测 (GDS) 来研究东部CAOB下方的深度电导结构.
- 了解深层结构与该地区广泛传播的岩石源之间的关系.
主要方法:
- 地磁观测站数据收集和处理.
- 对于C-响应曲线的受限影响远程参考 (BIRRP) 处理.
- 渐变的网格有限差异向前建模.
- 在球形坐标中使用有限内存准牛顿方法 (L1-规范) 进行3D反转.
主要成果:
- 获取地下3D电导率模型.
- 在蒙古-奥霍茨克线下的MTZ内发现了两个显著的高导电率异常.
- 这些异常与该地区的地质和岩历史的相关性.
结论:
- 高导电性异常很可能代表停滞的海洋地或分层的岛屿弧形材料.
- 在MTZ中下降的板块或石质层残留物被推断导致热地幔材料的上游.
- 这种上升被认为是蒙古-奥霍茨克线两侧观测到的广泛火山岩的驱动力.
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