概括
大盆地经历了显著的地缩短和延伸,需要修订的地质重建. 新的分析揭示了至少104-135公里的缩短和250公里的延伸,重塑了我们对其原生代到早期坎布里亚盆地的理解.
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
- 结构地质学 结构地质学
背景情况:
- 大盆地对于了解前生代和古生代地质学和地力学至关重要.
- 由于新的数据,以前对中生代和中生代变形历史的重建需要修改.
研究的目的:
- 为大盆地的中期原生代到早期坎布里亚岩石开发新的palinspastic重建.
- 为了整合关于中生代-中生代地缩短和延长的新发现,以准确的区域背景.
主要方法:
- 分析地质证据,证实地通过东向向的推力和折叠缩短.
- 古磁数据限制了自中生纪晚期以来的延伸方向和大小.
- 地质和古磁不确定性被用来估计与度的延伸变化.
主要成果:
- 据估计,地的总缩短距离为104至135公里.
- 大约250公里的延伸发生在大盆地.
- 原始的Proterozoic和早期坎布里亚盆地宽度为150至300公里,更朝南朝北.
结论:
- 对大盆地的地质历史进行修订的重建是必要的.
- 该地区经历了大量的缩短和延伸,显著改变了其古地理.
- 古磁数据支持最小的塞拉内华达旋转,简化了延伸计算.
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