概括
肯塔基州梅斯维尔附近的新地质层被认为是科普形成. 这种新的名称避免了Eden这个术语,因为它具有阶段性意义,澄清了岩石单位的相关性.
科学领域:
- 地质地质地质地质地质地
- 在平流图学中,平流图学.
- 古生物学的古生物学
背景情况:
- 肯塔基州梅斯维尔附近的岩层与辛辛那提的伊甸园和较低的费尔维尤岩层有相似之处.
- "伊甸园"这个术语带有阶段性内涵,因此需要修订命名法,以提高清晰度.
研究的目的:
- 为肯塔基州梅斯维尔附近的岩层提出一个新的地质形成名称.
- 为了建立明确的平流图相关性,避免模两可的术语.
主要方法:
- 位于肯塔基州梅斯维尔附近的岩石单位的战略分析.
- 根据石质学和地平面位置,对科佩岩层形成的定义.
主要成果:
- 拟议的科普形成由中层石页岩组成,平均粘性比为2.5至3.8.
- 这些页岩相应地覆盖了Pleasant石灰岩 (平均粘性比为1.0) 和未命名的页岩石灰岩 (平均粘性比为0.5).
结论:
- 科普形成为这些岩石单元提供了一个独特而明确的名称.
- 这种重新定义使梅斯维尔-辛辛那提地区的地质相关性更为精确.
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