在美国加利福尼亚州内华达山脉南部下方拍摄的土石化层
Oliver S Boyd1, Craig H Jones, Anne F Sheehan
1Department of Geological Sciences, University of Colorado at Boulder, 2200 Colorado Avenue, Boulder, CO 80309-0399, USA. oliver.boyd@colorado.edu
概括
地震断层扫描显示了深层石质层,包括生态石和石榴石石,在内华达山脉下面下降. 这揭示了该地区连贯的石质层移除过程.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 塞拉内华达山脉有一个复杂的地质历史.
- 了解石质层结构和动态对于板块构造学至关重要.
研究的目的:
- 为了研究位于内华达山脉东南部的深层石质层结构.
- 描述下降岩层的组成和几何形状.
主要方法:
- 地震断层扫描被用于图像地下结构.
- 对地震波速度的分析,以推断材料的特性.
主要成果:
- 观测到富含石榴石的地和地幔石化层下降到上层地幔.
- 下降的石化层由两个不同的层组成:上面的富含铁的生态石矿,上面的富含的石榴石矿.
- 下降的生态石位于之前在南方大谷中识别的高P波速度材料上方.
结论:
- 这些发现表明,在塞拉内华达山脉和大谷下方的石质层移除过程中,存在以前未知的连贯性.
- 这项研究为大陆石灰岩层的沉降和同化提供了新的见解.
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