概括
在生态中的克林诺素因位置和分布而有很大的不同. 低度 (<少数ppb) 表明可能是污染物,而不是矿物固有的.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 放射性同位素地质学 放射性同位素地质学
背景情况:
- 生态岩石是理解地球深层过程的关键岩石类型.
- 克林诺皮洛克森是许多生态矿石中的主要矿物.
- 矿物中的分布为地质过程提供了洞察力.
研究的目的:
- 为了研究的度和分布在生态的clinopyroxenes.
- 为了确定这些矿物中的不同发生方式.
- 为了将含量和分布与地质环境相关联.
主要方法:
- 用裂变轨道分析来研究.
- 分析了来自四个不同的地质遗址的分离的clinopyroxene样本.
- 的度和分布模式 (集群,裂,均) 的特征.
主要成果:
- 的发生包括集群,裂纹相关线条和均分布.
- 均度的样本内变化范围从2x到4x.
- 平均均度的地点间变化范围约为1000x (0.0120 ppb).
- 来自海洋盐湖石坑遗址的克林诺普罗素显示了最高的 (1520 ppb) 和最均的分布.
结论:
- 分布在生态的clinopyroxenes是高度可变的,受地质位置的影响.
- 在clinopyroxenes中低度 (<少数ppb) 可能代表外部污染物.
- 该研究强调了考虑的发生模式对于准确的地化学解释的重要性.
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