德克萨斯州中部的Silurian:该地区的第一个记录
概括
在德克萨斯州中部的Llano提升中发现了新的Silurian Starcke石灰岩突出. 这些以前未被记录的地质构造在埃伦伯格集团的崩结构中发现.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 在平流图学中,平流图学.
背景情况:
- 在德克萨斯州中部,丝纪的岩石形成很少.
- 拉诺高原是理解区域层结构的一个关键地质区域.
研究的目的:
- 为了记录在德克萨斯州中部发现以前未被记录的西卢里亚时代的发现.
- 为了描述新发现的Starcke石灰岩形成.
主要方法:
- 地质场地图和岩石突出物识别.
- 岩石形成的平流图分析.
- 化石收集和年龄的确定.
主要成果:
- 在Llano升起的崩塌结构中确定了Silurian突起.
- 这座名为Starcke石灰岩的新岩层是一种粉红灰色的颗粒状石灰岩.
- 化石表明斯塔克石灰岩的温洛克可能年龄.
结论:
- 斯塔克石灰岩的发现代表了德克萨斯州这一地区第一次记录西卢里亚时代的浮点.
- 斯塔克石灰岩提供了新的洞察力地质历史和沉积环境在Silurian时期Llano提升.
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