概括
莫加尼特是一种罕见的二氧化多态,在全球各种石英样本中占有很大一部分 (10-80%). 它的存在和分布在石英品种中,如石和石,为地质环境和流体岩石相互作用提供了见解.
科学领域:
- 矿物学是什么?矿物学是什么?
- 地质化学 地质化学
- 晶体学 晶体学是指结晶学.
背景情况:
- 石英是一种常见的二氧化多态体,但其不太知名的多态体莫加尼特被低估了.
- 以前的研究还没有完全量化莫加尼特在各种石英品种中的流行程度.
研究的目的:
- 在世界各地的各种细粒度石英样本中调查莫加尼特的存在和丰富性.
- 探索莫加尼特作为特定地质条件和过程的指标的潜力.
主要方法:
- 对150多个石英样本进行了X射线检查.
- 瑞特维尔德对50个纤维石英和非纤维石英的粉末X射线衍射模式进行了精细分析.
主要成果:
- 石英样本中的摩加尼特含量在10%至80%之间.
- 在来自干旱,性环境的桃中发现了高度的摩加尼特 (> 30%).
- 摩加尼特在经过气候变化和水热变化的二氧化样本中显著缺席.
结论:
- 莫加尼特是细粒度石英的广泛组成部分,通常存在大量.
- 桃中莫加尼特的存在可能表明过去的蒸发模式.
- 莫加尼特的缺失可以作为流体岩石相互作用和变化过程的代理.
相关概念视频
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