在科罗拉多高原下方的一个米奥森石化层滴水的盆地记录
1Department of Geoscience, University of Arizona, Tucson, AZ, 85721, USA. johnhe@arizona.edu.
Nature communications
|July 22, 2023
概括
在科罗拉多高原下方的石质层沉降导致了动态升起,记录在古代的比达霍奇盆地. 这项研究揭示了地质过程如何随着时间的推移塑造表面地形.
科学领域:
- 地动力学和构造学
- 沉积地质学 沉积地质学
- 同位素地球化学 同位素地球化学
背景情况:
- 高海拔高原通常由沉降的石化层升起.
- 数字模型表明,这一过程创造了沉积物记录中保存的动态地形.
- 这种现象的记录实例很少见.
研究的目的:
- 调查科罗拉多高原的石质层滴水和表面提升之间的联系.
- 为了分析米奥森Bidahochi盆地的沉积记录,寻找动态地形的证据.
- 整合地质物理,地质化学和地质数据,以了解高原升起机制.
主要方法:
- 对U-Pb,Lu-Hf和微量元素数据的分析.
- 在比达霍奇盆地附近的岩石岩石的地球化学和同位素分析.
- 地质物理,地化学和地质证据的整合.
主要成果:
- 比达霍奇盆地保留了准圆形表面对岩层滴水反应的记录.
- 系统的同位素,地化学,温度和fO2过渡在近接岩层中被观察到.
- 证据支持空间和时间变化的沉降和升起记录,与石质层滴水模型相一致.
结论:
- 在科罗拉多高原,可以识别由石质层滴水驱动的动态地形.
- 这些发现支持了在厚厚的石质层高原下逐渐滴水的模型.
- 这项研究表明,在单个石层滴水的规模上,动态地形的保存.
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