通过同步双重推进来调和长期地形增长的模式与共同地震提升
Yuqing Zhang1,2,3, Hanlin Chen4,5, Xuhua Shi6,7,8
1Research Institute of Petroleum Exploration and Development, PetroChina, Beijing, China.
长期的山岳建筑涉及同步断层推进,解释了表面升起和河流露台折叠. 这揭示了断层系统的进化如何在数百万年内塑造地形.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地质形态学 地质形态学
背景情况:
- 了解长期地形变化和共地震提升之间的联系对于积极的山面演变至关重要.
- 地质时间尺度上的表面变形和断层活动之间的关系仍然是一个关键的辩论.
研究的目的:
- 为了研究表面地形变化和使用Pishan双重系统的重震升起之间的关系.
- 模拟生长层和河流露台折叠的发展,以了解断层动力学.
主要方法:
- 模拟生长层的发展和河流露台的折叠.
- 分析具有不同滑动率的邻近断层的双重推进.
- 研究Pishan推力系统的顺序传播.
主要成果:
- 为了解释观察到的生长层和露台折叠,需要对具有不同滑动率的两个断层进行同步推进.
- 模拟了露台折叠和相反的浸泡增长层面板的流入盆地的迁移.
- 调和了长期露台变形和短期振荡升高之间的差异.
结论:
- 不同时间尺度的地形不匹配反映了断层系统的长期动力演变.
- 描述地下断层动力学对于研究山脉带的地形增长至关重要.
- 在全球范围内,重新思考活跃的折叠和推力带中的山地形成过程受到这些发现的激励.
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