概括
沿北美东部的近似时间对应的纪沉积物.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 沉积物学的沉积物学
背景情况:
- 地震反射地平线A沿北美东部海岸确定.
- 与地平线A相关的沉积物是晚期-早期-早期-中期伊欧时的年龄.
- 这些沉积物含有非原生矿物质,表明火山玻璃的变化.
研究的目的:
- 调查陆上有质沉积物的起源.
- 为了确定陆上沉积物是否与地平线的海上沉积物相关,A.
- 为了在陆上和海上地质构造之间建立火山联系.
主要方法:
- 纪沉积物的沉积物学分析.
- 矿物学检查以确定异性矿物质.
- 陆上沉积物与海上地震数据的相关性 (A地平线).
主要成果:
- 亚特基因矿物套件表明,埃奥森时期沉积物中的火山玻璃发生了变化.
- 陆上性沉积物与离岸地平线A的时间相当.
- 矿物学支持质沉积物的火山起源.
结论:
- 陆上的质沉积物与海上地平线A的石有着共同的火山起源.
- 火山玻璃的变化是形成这些纪沉积物的关键过程.
- 建立了陆上和海上Eocene形成之间的重要地质联系.
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