北美克拉顿的石化层层
Huaiyu Yuan1, Barbara Romanowicz
1Berkeley Seismological Laboratory, 209 McCone Hall, Berkeley, California 94720, USA.
Nature
|August 27, 2010
概括
稳定的大陆格有两个不同的石化层,而不是一个. 这一发现解决了地震和地化学数据之间的差异,揭示了中层石灰岩层的边界.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
背景情况:
- Kratons 是古老的,稳定的大陆地区域,它们的形成和保存数十亿年来是一个重要的地质辩论.
- 地震接收器功能的研究已经确定了一个浅层的结构边界在克拉顿下面,与传统的石化层-石化层边界 (LAB) 不一致.
研究的目的:
- 用地震异构学研究北美大陆石化层的结构.
- 为了调和冲突的地质物理和地化学数据关于cratonic石化层结构.
主要方法:
- 对地震波的亚齐木斯特异性随着深度的变化进行分析.
- 地震数据与来自石热气流分析的地化学推断的比较.
- 集成地震学,地质化学和地力学数据.
主要成果:
- 证据表明北美大陆有两个不同的岩层层,通过亚齐木斯特异性确定.
- 上层的厚度与高度耗尽的化学层相关.
- 存在一个相对平坦的石化层-石化层边界 (180-240公里深),可能是围绕枯竭层的热根.
结论:
- 检测到的浅层地震边界可能代表了中层岩层边界,而不是LAB.
- 这些发现整合了多样化的数据集,为北美岩层提供了一个统一的模型.
- 这项研究阐明了古代大陆石化层的复杂结构和演变.
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