概括
长达660公里的地幔不连续性是由马脊柱石 (环木石) 的分解引起的. 新的激光加热钻石天细胞实验证实了这种过渡发生在地球地幔压力下,使地震数据与矿物物理相协调.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 高压地质化学 高压地质化学
背景情况:
- 这660公里的地震不连续性被归因于马脊柱石 (环木石) 分解成MgSiO3-矿和矿.
- 之前的研究对这种过渡发生的压力提出了相互矛盾的数据,挑战了既有的地幔组成模型.
研究的目的:
- 为了准确地确定660公里地幔深度的马螺旋分解的压力和温度条件.
- 解决关于660公里不连续性的地震观测和矿物物理数据之间的差异.
主要方法:
- 在现场使用激光加热的钻石细胞进行X射线衍射.
- 精确控制压力,温度和水静态条件.
- 在高压,高温条件下对玛-Mg2SiO4相变的分析.
主要成果:
- 玛-Mg2SiO4保持稳定,压力和温度相当于660公里深 (24GPa,1,900 K).
- 分解产物被确定为MgSiO3-矿和MgO (氧化物).
- 实验结果与地震数据一致,解决了之前的差异.
结论:
- 660公里的地震不连续性与在地质学上相关的条件下马脊柱的分解相一致.
- 准确的压力和温度测量对于将矿物物理与地震学相协调至关重要.
- 地球地幔的矿物学模型得到了这些发现的支持.
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