海平面的变化. 遗传的景观和海平面变化
Sierd Cloetingh1, Bilal U Haq2
1Utrecht University, Utrecht, Netherlands.
概括
地质物理学和沉积地质学现在汇聚在一起,将地球连接起来.
科学领域:
- 整合地质物理学和沉积地质学,以统一理解地球的动态过程.
- 专注于岩层记忆和影响表面地形的地幔动力学.
背景情况:
- 板块构造学最初专注于海洋地,在解释陆地地形异常方面取得了有限的成功.
- 传统的地质物理学努力模拟垂直运动和地球深层结构.
- 沉积地质学缺乏对盆地演变和沉积预算的整体方法.
研究的目的:
- 为了弥合地质物理学和沉积地质学之间的差距.
- 解释板内部和大陆边缘令人费解的地形特征.
- 整合对地球深层和表面过程的理解.
主要方法:
- 先进的地球物理成像用于建模深层结构和垂直运动.
- 石质层机械性质的量化.
- 源至沉沉沉积系统的定量建模和整体整合.
主要成果:
- 建立了石质层记忆,作为地质物理学和沉积地质学之间的连接纽带.
- 更好地了解地幔动力学是如何通过石层转移到表面的.
- 能够重建过去的地质景观和盆地演变.
结论:
- 地质物理学和沉积地质学的融合正在彻底改变地球科学.
- 石质层记忆为理解表面地形提供了一个统一的框架.
- 先进的定量方法提高了我们重建地球历史的能力.
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