地球地幔中的弱立方CaSiO矿
J Immoor1, L Miyagi2, H-P Liermann3
1Bayerisches Geoinstitut (BGI), University of Bayreuth, Bayreuth, Germany.
Nature
|March 10, 2022
概括
立方酸盐 (CaSiO3) 矿是一种较弱的地幔下相. 它的低强度和粘度可能决定了压力板的动态,并解释了地震异常.
科学领域:
- 地质学
- 矿物物理
- 高压地质化学
背景情况:
- 立方CaSiO3矿在~550公里的海底地中形成.
- 它在地幔下部的质性质尚不清楚.
研究的目的:
- 为了研究立方CaSiO3矿的塑性强度和质性行为.
- 确定其在压力板动态和下层结构中的作用.
主要方法:
- 对立方CaSiO3矿的塑料强度测量
- 在高压和高温下进行模拟,模拟地幔下层条件 (深度可达1200公里).
主要成果:
- 在较低的地幔温度下,立方CaSiO3矿明显弱于桥矿和铁烯酸.
- 它的强度和粘度比其他主要的下层层相低得多.
- 这可能是地幔下层最弱的阶段.
结论:
- 薄弱的立方CaSiO3矿可能控制了压缩板的动态.
- 它提供了将海洋地与地幔分离的机制.
- 可能解释最上层的下层地幔和核心地幔边界的低地震速度区域.
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