概括
在阿巴拉契山脉的阿勒根山地质形成是由左侧转压和冈德瓦纳旋转造成的,而不仅仅是斜碰撞. 这种新模型解释了阿巴拉契亚山脉,奥阿奇塔山脉和瓦里斯基德山脉的融合和断层.
科学领域:
- 地质地质地质地质地质地
- 板块构造学是一种板块构造学.
- 结构地质学 结构地质学
背景情况:
- 传统上,阿勒根亚山脉形成的原因是刚德瓦纳和劳伦西亚之间的右侧斜碰撞.
- 这种模型无法解释Ouachitas和Variscides的同时代融合,并且与阿巴拉契亚山脉的构造运输指标相矛盾.
研究的目的:
- 提出一个替代的动力学模型的阿勒根亚州的orogeny.
- 为了协调来自阿巴拉契亚山脉,奥阿希塔斯山和瓦里斯基德山的地质证据.
主要方法:
- 动力学建模 动力学建模
- 对构造运输指标的分析.
- 地质数据的整合.
主要成果:
- 拟议的模型涉及阿巴拉契亚山脉早期的左侧转压.
- 它包括刚德瓦纳的反时钟旋转.
- 这导致了从南欧到阿拉巴马州的右侧冲击滑动断层的形成.
结论:
- 亚勒根人土生态更好地解释为左侧转压的模型,其次是冈德瓦纳旋转.
- 这种修订后的动力学模型为在多个orogenic带中观察到的地质特征提供了更全面的解释.
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