非海洋白-第三纪边界地区的地质框架,老鼠盆地,新墨西哥州和科罗拉多州
概括
高的度被发现在白纪-第三纪的边界在拉顿盆地. 这一发现与拉顿岩层内的特定粘土岩层有关,表明了重要的地质事件.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学
- 沉积地质学 沉积地质学
背景情况:
- 甲-第三纪 (K-T) 边界标志着地球历史上一个重要的灭绝事件.
- 异常常常与外星撞击有关,例如奇克苏鲁布撞击事件.
- 河流沉积岩提供了对陆地古环境的独特见解.
研究的目的:
- 为了调查古学白-第三纪边界的异常度.
- 描述拉顿盆地异常的地质背景.
- 为了将发现与潜在的外星事件标记者相关联.
主要方法:
- 对沉积岩样本进行地质化学分析以确定的度.
- 为了准确地确定白-第三纪的边界,进行了古生物学分析.
- 战略记录记录和河流沉积岩的描述. 在鼠标形成.
主要成果:
- 在白纪-第三纪边界检测到异常高的度.
- 异常在空间上与薄薄的高酸粘土石床有关.
- 这种粘土石是在较低的拉顿岩层中不连续的碳状页岩和煤炭序列中发现的.
结论:
- 在老鼠盆地检测到的异常支持了外星事件影响陆地生态系统的假设.
- 与特定的石质结构 (高酸粘土石,碳酸页岩,煤炭) 的关联为沉积环境提供了线索.
- 需要进一步的研究,以充分理解这种异常对北美KT边界事件的影响.
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