来自南方阿巴拉契亚半岛变态岩石的密西西比化石及其对晚期古老生态时代构造进化的影响
概括
在阿拉巴马州的塔拉德加石板带中发现的密西西比化石表明,变形发生的时间比以前认为的要晚. 这一发现需要重新评估南部阿巴拉契亚山脉的构造历史.
科学领域:
- 古生物学和平流图学.
- 结构地质学和构造学
背景情况:
- 阿拉巴马州的塔拉德加石板带,是西部蓝带的一部分,此前被认为在阿卡迪亚的orogeny期间经历了变形和变形.
- 现有的解释表明,这些地质事件发生在早期碳化时期之前.
研究的目的:
- 为了确定塔拉迪加石板带内的变形和变形的更精确的年龄.
- 根据新的化石证据,重新评估最南端的阿巴拉契亚山脉的构造历史.
主要方法:
- 从埃林石板中回收和识别化石,特别是Periastron reticulatum,从埃林石板.
- 层级分析以确定化石含岩层的地质年龄.
主要成果:
- 关于Periastron reticulatum Unger的化石进行了修订. 贝克被恢复,建立一个密西西比 (Kinderhookian-Tournaisian) 时代的埃林石板.
- 这种年龄表明,塔拉迪加石板带的变形和变形发生在早期碳化 (阿莱加尼亚) 之后.
结论:
- 新的化石数据与此前对该地区阿卡迪亚山脉形成时间的解释相矛盾.
- 需要对最南端的阿巴拉契亚山脉的构造进化进行修订的理解,考虑到早期碳岩时期后的变态和变形事件.
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