概括
阿根廷南部的冰川冰延伸到远东,在岩流之间沉积到床. 最古老的塔尔可以追溯到320万年前,而最年轻的塔尔是170万年前.
科学领域:
- 地质地质地质地质地质地
- 古气候学 古气候学
- 火山学 火山学是一门学科.
背景情况:
- 阿根廷南部的地质记录揭示了过去冰川活动的证据.
- 相互交织的岩流和田间沉积物提供了对区域环境历史的洞察力.
研究的目的:
- 迄今为止,阿根廷南部的冰川床.
- 重建该地区过去冰川事件的程度和时间.
主要方法:
- 地质地图绘制到床和交叠的岩流.
- 与田地沉积物相关的火山层的放射测年.
主要成果:
- 蒂尔床是由冰层沉积的,冰层至少从现在的山脉山脊以东延伸40公里.
- 封顶最古老的床的岩流可以追溯到320万年±100万年前.
- 最年轻的床被一个流动的岩覆盖,年龄约为170万年±50万年.
结论:
- 在平世-平世时期,冰川冰在阿根廷南部显著向东推进.
- 岩流的约会为该地区的冰川事件提供了一个时间框架.
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