概括
大盆地的世地下水补充变得枯竭了. 这种转移在石灰质静脉中得到证实,与影响太平洋风暴系统的主要山脉的升起有关.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 水文学 水文学
背景情况:
- 地质构造中的液体含量保留了古老的环境条件.
- 水中的含量反映了它的来源和蒸发或降水的历史.
- 普莱斯托时代是气候和地质变化的重要时期.
研究的目的:
- 为了重建过去的地下水填充条件在南部大盆地.
- 为了研究构造上升对古水文学的影响.
- 了解地形效应对降水中的含量的影响.
主要方法:
- 系列测年静脉,以建立一个时间框架.
- 分析这些静脉内的液体含量,以确定含量.
- 地质和气候学建模以解释同位素变化.
主要成果:
- 记录了地下水补充中的含量每毫升40的显著减少.
- 这种同位素转移发生在普世时期.
- 时间与塞拉内华达山脉和横跨山脉的主要升起事件相关.
结论:
- 南部大盆地的地下水补充在普莱斯托纪期间经历了大量的耗.
- 山脉的升起可能加剧了太平洋风暴造成的的形枯竭.
- 这项研究强调了构造学,气候和水文同位素特征之间的联系.
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