概括
科特迪瓦 tektites 包含一个小的石组成部分,可用 rhenium-osmium (Re-Os) 同位素分析检测. 这种方法非常适合研究石对古代地的影响,因为它具有明显的同位素特征和线性混合趋势.
科学领域:
- 地质化学 地质化学
- 宇宙化学 宇宙化学
- 行星科学 行星科学
背景情况:
- 泰克石是石撞击过程中形成的天然玻璃.
- 象牙海岸的石头起源于博斯姆特维湖的冲击结构.
- 仅仅对贵金属的分析不足以检测这些铁矿石中的石成分.
研究的目的:
- 为了量化象牙海岸 tektites 的石成分.
- 评估- (Re-Os) 系统在石撞击研究中的实用性.
- 为了分析tektites和源岩中的Os同位素组成.
主要方法:
- 测量 (Re) 和 (Os) 的度.
- 对Os同位素组成的分析.
- 德基石和目标岩石 (博斯姆特维湖) 组成的比较.
主要成果:
- 科特迪瓦 tektites 包含大约0.6%的石组成部分.
- Re-Os同位素系统提供了一种强大的方法来检测石贡献.
- 原子的同位素组成是对冲物质的可靠指标,即使有元素损失.
结论:
- Re-Os系统对于识别石撞击事件在旧大陆地上是非常有效的.
- 冲击物和目标岩石的不同同位素组成对于这种方法至关重要.
- 在Re-Os的同位素图表上线性混合有助于识别撞击后的元素移动性.
相关概念视频
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For instance, group IV...
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