古登伯格的不连续性:在石化层-石化层边界化
1Department of Terrestrial Magnetism, 5241 Broad Branch Road, NW, Washington, DC 20015, USA. nschmerr@dtm.ciw.edu
概括
海底的古登堡不连续性 (G) 可能是由石化层底部的部分融化引起的. 这种地震信号被地幔动力学增强,如上升和俯冲.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地幔动力学地幔动力学
背景情况:
- 石化层-石化层边界 (LAB) 将刚性板块与对流地幔分开.
- 根特堡不连续性 (G) 的起源,在LAB的地震不连续性,是不太了解.
研究的目的:
- 为了调查海洋板下古堡不连续性 (G) 的原因.
- 为了确定石化层-石化层边界 (LAB) 的部分融化是否解释了G反射性.
主要方法:
- 分析高频SS前体的地震数据.
- 在太平洋板下40-75公里深处间歇检测G作为负速度对比.
主要成果:
- 在火山活动和化生产的地区,在LAB附近观察到G.
- 观测结果与石质层底部间歇性层次的星球部分融化相一致.
结论:
- 古登堡断续性 (G) 可能是由于石化层-石化层边界 (LAB) 的部分融化造成的.
- 由于地幔的上升,小规模的对流,以及在潜水过程中释放的流体,融的产生得到了增强.
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