概括
在加利福尼亚州的Diagenetic克里斯托巴莱特.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 沉积岩石学 沉积岩石学
背景情况:
- 加利福尼亚州的蒙特利页岩形成.
- 多态的二氧化的基因变化.
- 克里斯托巴莱特的结构和特性
研究的目的:
- 调查基因基因cristobalite中的结构变化.
- 在不同的埋葬深度分析蒙特利页岩中的克里斯托巴莱特.
- 在chert中比较克里斯托巴莱特和陶.
主要方法:
- 进行X射线衍射 (XRD) 分析.
- 测量d(101) 间距的测量
- 来自不同埋葬深度的矿物样本的比较.
主要成果:
- 观察到d(101) 间距从4.115到4.040英尺的间距下降,随着埋葬深度的增加.
- 陶岩中的克里斯托巴莱特比相关的chert表现出较小的d(101) 间距 (0.0040.015安格斯特姆).
- 在cristobalite中逐渐发生结构变化的迹象.
结论:
- 埋葬深度对克里斯托巴莱特的内部结构产生重大影响.
- 后来在器石中形成的克里斯托巴莱特可能解释了结构上的差异.
- 了解二代遗传过程对于解释二氧化二代遗传至关重要.
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