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Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey最新文献

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A Simple Model for Plate Motion and Topography 板块运动和地形的简单模型
Pub Date : 2024-07-11 DOI: 10.25288/tjb.1459797
Ö. Bodur
The traditional explanation of slow dynamic subsidence and uplift of tectonic plates solely depends on the vertical motion of mantle density anomalies. This has been challenged by observations of rapid and short-lived elevation changes exceeding 100 meters per-million-year in numerous sedimentary basins. Bodur et al., (2023) have shown that relative tectonic plate motion and associated basal shear stress can explain those rapid and short-lived elevation changes. In this paper, I suggest a basic approach to quantify elevation changes resulting from basal shear stress by employing torque-balance calculations. The results confirm the existing flow model solution and offer a more robust formula for estimating the impact of plate motion on changes in Earth's topography. Such functionality may prove invaluable in various applications including interpretation of stratigraphic records.
对构造板块缓慢动态沉降和隆起的传统解释完全依赖于地幔密度异常的垂直运动。但在许多沉积盆地中,观测到的每百万年超过 100 米的快速而短暂的海拔变化对这一解释提出了挑战。Bodur 等人(2023 年)指出,相对构造板块运动和相关的基底剪应力可以解释这些快速而短暂的海拔变化。在本文中,我提出了一种基本方法,通过扭矩平衡计算来量化基底剪应力导致的海拔变化。结果证实了现有的流动模型解决方案,并为估算板块运动对地球地形变化的影响提供了一个更稳健的公式。这种功能在包括地层记录解释在内的各种应用中可能会被证明是非常有价值的。
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Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey
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