东南极洲Dome Fuji地区的构造结构,基于新的磁性数据
Alexandra Guy1, Graeme Eagles2, Olaf Eisen3,4
1Czech Geological Survey, Prague, Czech Republic.
Scientific reports
|August 10, 2024
概括
最古老的冰川侦察调查揭示了东南极洲的新冰川下地质细节. 这些发现提供了对超大陆罗丁尼亚和冈德瓦纳的构造历史的见解.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地质地质地质地质地质地
背景情况:
- 东南极冰盖隐藏着重要的地质信息.
- 了解亚冰期地质学有助于重建超大陆组合.
研究的目的:
- 通过使用空中地质物理学来研究福建圆顶地区的冰下地质.
- 为罗丁尼亚和冈德瓦纳的构造历史提供新的见解.
主要方法:
- 进行了最古老的冰川侦察 (OIR) 空载地质物理调查 (2016/17).
- 整合了新的磁性和雷达衍生床地形数据与现有的磁性和重力数据.
- 分析磁性,重力和地形数据,绘制地领域的地图和识别地质结构.
主要成果:
- 在调查区域内绘制了由NS边界划分的三个不同的地领域.
- 确定了与地形和重力模式相关的四组磁线.
- 标志着东尼洋弧超级地形 (TOAST) 的南向延续,并建议埃尔伯特磁异常作为瓦尔基里克拉顿和TOAST之间的接.
- 揭示了OIR剪切区域,由Ruker和Valkyrie坑在冈德瓦纳合并期间的斜碰撞形成.
结论:
- 该OIR调查显著提高了对东南极的亚冰川地质学的理解.
- 结果为罗丁尼亚和冈德瓦纳的构造进化和超大陆周期提供了关键证据.
- 确定了像OIR剪切区这样的地质特征,为大陆合并过程提供了新的视角.
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