相关实验视频
Updated: Jul 12, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
在南澳大利亚,晚伊欧纪火山灰转化为珀-CT,反映了全球沉积物. 这表明,在此期间,澳大利亚南部有广泛的火山活动.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 火山学 火山学是一门学科.
背景情况:
- 位于南澳大利亚的布兰奇点岩层包含了交替的硬层和软层.
- 这些层是由火山灰,海绵和化石遗骸组成的.
- 选择性化后来形成了硬层.
研究的目的:
- 分析布朗什点形成的组成和起源.
- 为了将这些南澳大利亚矿床与全球类似的地质构造进行比较.
- 为了推断埃奥森晚期火山活动的程度和原因.
主要方法:
- 对Gull Rock和Tuit成员的沉积物分析.
- 地质化学研究矿物质改变过程.
- 与白纪和纪沉积物进行比较的平流学.
主要成果:
- 火山灰的改变产生了斯麦克提特和克林诺皮托利特,释放了二氧化.
- 结晶为珀-CT,形成了硬层.
- 从新西兰到西澳大利亚发现了类似的沉积物.
结论:
- 改变过程在不同地理位置上是一致的.
- 澳大利亚南部发生了广泛的晚伊欧纪火山活动.
- 这种火山活动与南极洲的裂和分离有关.
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