在构造板下部分融化的地震证据
Eric Debayle1, Thomas Bodin2, Stéphanie Durand2
1Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, Villeurbanne, France. Eric.Debayle@ens-lyon.fr.
Nature
|October 22, 2020
概括
部分融化存在于上层地幔的地震低速区 (LVZ),为天气层提供食物. 这种融化率低于0.30%,促进了构造板块的运动和晶体的对齐.
科学领域:
- 地质学
- 地幔动力学
- 地震学
背景情况:
- 上层地幔的地震低速区 (LVZ) 对板块构造学至关重要,但其起源仍有争议.
- 现有理论提出部分融化,固态机制或挥发性含量是低地震速度的原因.
研究的目的:
- 使用剪切减弱和速度模型调查低速度地震区 (LVZ) 的起源.
- 为了确定LVZ内部分融化的存在和分布.
主要方法:
- 全球三维剪切衰减模型的解释.
- 全球三维地震速度模型的解释.
主要成果:
- 在海洋LVZ内部分融化的证据,在中海山脊,热点和后方弧线区域下方150-200公里.
- 只有不到0.30%的融化物被困在海洋的LVZ中;在大陆下大部分没有融化物.
- 融化的度随着板块的速度而增加,特别是在每年3-5厘米之间.
结论:
- 部分融化是海洋上层地幔的重要组成部分.
- 融化降低了层粘度,促进了板块的运动和大规模的地幔晶体对齐.
- 发现支持融化的作用在板块与地幔脱.
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