在塔塔豪因石中碳酸盐的形成
J A Barrat1, P Gillet, C Lécuyer
1Université d'Angers, Laboratoire de Géologie, 2 Boulevard Lavoisier, 49045 Angers Cedex, France.
概括
塔塔豪因石显示了陆地污染,由二次石矿物质和棒形形式的证据证明,在地球暴露63年后,在断裂上出现. 碳同位素分析证实这些特征起源于地球,而不是石本身.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 行星科学 行星科学
背景情况:
- 石提供了对外星物质和过程的洞察.
- 随着时间的推移,陆地污染会改变石的组成.
- 1931年,塔塔豪因石在突尼斯落下.
研究的目的:
- 为了调查塔塔霍因石的陆地污染.
- 描述二级矿物质和石碎片上形成的形式.
- 为了确定这些次要特征的起源.
主要方法:
- 对不同时间收集的石样本进行比较分析.
- 微镜检查骨折的二次矿物质生长.
- 对石和周围土壤中的碳酸盐进行碳同位素分析 (δ13C PDB).
主要成果:
- 1931年的石样本显示有断裂,但没有二次矿物质.
- 1994年的样本显示了骨折上的石聚合物和棒状形式.
- 二次碳酸盐的碳同位素值与陆地土壤的碳同位素值相匹配,表明地球起源.
结论:
- 塔塔豪因石在地球上63年的时间里经历了显著的陆地污染.
- 由于陆地气候变化,二次石和相关的微观结构在降落后形成.
- 同位素分析是一种可靠的方法,用于在石中区分地外物质和地球物质.
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