相关实验视频
Updated: Jun 4, 2026

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
评论"地幔流驱动海洋板块的沉降"
Marcel B Croon1, John K Hillier, John G Sclater
1Scripps Institution of Oceanography, University of California, San Diego, 9500 Gilman Drive, San Diego, CA 92093-0220, USA. mcroon@ucsd.edu
概括
这项研究挑战了海底深度取决于距离中洋山脊的距离的观点. 相反,数据表明深度与年龄的关系,质疑地幔流在海底沉降中的作用.
科学领域:
- 地质物理学 地质物理学
- 海洋地质学海洋地质学
- 板块构造学是一种板块构造学.
背景情况:
- 以前的研究提出了一个"地幔流线"模型,其中海底深度随着距离中洋山脊的距离而增加.
- 这种模型建议地幔流作为海底沉降的主要驱动因素.
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