概括
加拉帕戈斯山丘的热水系统,超过30万年,已经从生产低沉积物转变为有限的富含的沉积物,表明随着时间的推移强度下降.
科学领域:
- 海洋地质学 海洋地质学
- 热水系统是热水系统.
- 地质化学 地质化学
背景情况:
- 加拉帕戈斯山丘是一个重要的海底热水系统.
- 了解这些土的演变,可以了解长期的地质过程.
研究的目的:
- 为了研究加拉帕戈斯山丘水热系统的年龄和沉积物组成.
- 确定系统活动和主导地位的历史变化.
主要方法:
- 来自加拉帕戈斯山丘领域的沉积物核心的分析.
- 对沉积物沉积物的地质化学分析以确定含量.
- 放射测年法用来确定系统的年龄.
主要成果:
- 加拉帕戈斯山丘的热水系统至少有30万年的历史.
- 较旧的沉积物缺乏,并且广泛覆盖了该地区.
- 目前的土沉积物以有限的丰富暴露为特征.
结论:
- 水热系统已经从以岩石为主导的系统转变为以水为主导的系统.
- 加拉帕戈斯山丘的热水系统的强度随着地质时间的推移而减少.
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