概括
在南极洲,南极洲是南极洲.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地质时间学 (Geochronology)
背景情况:
- 埃尔斯沃思山脉的地质历史对于理解冈德瓦纳的分裂至关重要.
- 以前的研究并没有完全限制该地区升起的时间和规模.
研究的目的:
- 为了确定埃尔斯沃思山脉上升的时间和规模,使用无裂变轨迹分析.
- 为了重建埃尔斯沃思山脉的构造历史在冈德瓦纳的碎片化背景下.
主要方法:
- 在Vinson Massif的4.2公里垂直截面的样本上进行了apatite裂变轨道分析.
- 热构造模型被用来解释裂变轨迹数据,并限制提升历史.
主要成果:
- 4公里或更多的升起发生在白纪早期,与韦德尔海的开放相吻合.
- 自白纪早期以来,至少保持了1.8公里的缓解.
- 自从白纪早期以来,已经发生了额外的3公里升起.
结论:
- 埃尔斯沃思山脉经历了与冈德瓦纳的分裂和韦德尔海的开放有关的显著的早期白纪升起.
- 埃尔斯沃思山脉的持续缓解表明正在进行的构造稳定性或随后的脱皮过程.
- 这些发现为西南极洲中新生代构造进化提供了关键的见解.
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