德纳利的晚期 cenozoic 提升及其与相对板块运动和断层形态学的关系
概括
丹纳利 (麦金利山) 经历了超过1公里/月的快速升起,从600万年前开始. 这座山脉形成是德纳利断层造成的.
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:
- 德纳利山 (麦金利山) 是北美最高的山峰.
- 了解主要山脉的构造历史对于地质研究至关重要.
研究的目的:
- 为了确定德纳利山脉升起的时间和速度.
- 为了调查山脉快速形成背后的因果因素.
主要方法:
- 在岩石样本上进行了阿帕蒂特裂变轨迹分析.
- 从德纳利山西侧的4公里的垂直部分采集了样本.
主要成果:
- 丹纳利山脉的快速升高 (> 1 公里/英里) 开始于大约 600 万年前.
- 升起是由德纳利断层的形态和太平洋-北美板块运动在5亿年前左右的变化驱动的.
- 沿断层的对立的触角运动向量迫使地块向上.
结论:
- 德纳利断层系统和板块构造变化是德纳利快速上升的关键驱动因素.
- 山的当前高度是相对较新的地质发展.
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