约瑟芬石中的Widmanstaetten图案,这是一个含金属的陆地岩石
概括
在陆地岩石约瑟芬石 (Josephinite) 中发现了Widmanstaetten图案,即缓慢冷却导致的溶解纹理. 这一发现表明约瑟芬石起源于地球的地幔.
科学领域:
- 地质地质地质地质地质地
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 约瑟菲尼特是一种独特的金属载体岩石,存在于蛇形化矿石层中.
- 陆地岩石通常不会表现出Widmanstaetten模式.
研究的目的:
- 为了调查约瑟芬石标本中Widmanstaetten模式的存在和起源.
- 为了确定约瑟芬石的热史和来源.
主要方法:
- 对来自俄勒冈州西南部的约瑟芬石标本进行显微镜检查.
- 分析金属相组合和脱溶质感的分析.
主要成果:
- 在变化较小的约瑟芬岩石区域中发现了Widmanstaetten模式,这是缓慢冷却溶解的特征.
- 散装成分表明最初的均金属存在于500°C以上.
- 这些模式在任何已知的陆地岩石中都是前所未有的.
结论:
- 观察到的Widmanstaetten模式为约瑟芬石的地幔起源提供了有力的证据.
- 约瑟菲尼特的热史与来自高温源的缓慢冷却一致.
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