概括
全新世化石珊瑚揭示了台湾的珊瑚.
科学领域:
- 地质和构造学地质学和构造学
- 海洋地球时间学 海洋地球时间学
背景情况:
- 台湾位于一个活跃的融合边缘,经历了复杂的构造相互作用.
- 升起的珊瑚礁为重建过去的海平面和构造活动提供了宝贵的档案.
研究的目的:
- 确定台湾三个不同构造区域的全新纪升起率.
- 调查板块碰撞对台湾垂直陆地运动的影响.
主要方法:
- 使用系列和碳-14 (14C) 同位素分析测定化石珊瑚样本的年代.
- 对海平面波动进行校正,以准确评估海拔变化.
- 在恒春半岛,东海岸山脉和离岸岛屿 (兰宇和卢陶) 上升率的比较.
主要成果:
- 台湾所有三个研究的地区都表现出Holocene升起.
- 沿着板块边界观察到明显更高的全新纪平均升起率.
- 东海岸山脉,一个板块边界,显示了最明显的升起.
结论:
- 板块碰撞是台湾高提升率的主要驱动因素.
- 该研究量化了台湾活跃边缘的构造上升的区域变化.
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