概括
上 Holocene 构造活动,包括折叠和提升,发生在西奈亚板的西部边缘 (Bardawil 湖) 和东部边缘 (伊拉特湾). 这些运动在区域构造学框架内进行分析.
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
- 四分学科学 四分学科学
背景情况:
- 西奈子板块在构造学上是活跃的.
- 上 Holocene 地质事件对于理解区域变形至关重要.
研究的目的:
- 为了研究在西奈亚子板沿线的上 Holocene 构造运动.
- 分析西部和东部边缘的折叠和提升活动.
- 将这些活动置于更广泛的区域构造框架内.
主要方法:
- 地质现场观测. 地质现场观测.
- 分析沿海的地形学.
- 构造框架解释. 构造框架解释.
主要成果:
- 在西奈亚子板的西部边缘,特别是在巴尔达维尔湖周围,发现了显著的折叠和升起运动.
- 提升也记录在东边缘的海岸,在伊拉特湾地区.
- 这些构造事件发生在上环新世时期.
结论:
- 西尼亚亚板的西部和东部边缘在上 Holocene 期间经历了相当大的构造活动.
- 观察到的折叠和升起与影响西奈子板的区域构造过程一致.
相关概念视频
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