大陆漂移引发了中国北部的早期珀姆纪干旱
Qiang Ren1,2,3, Shihong Zhang4, Mingcai Hou5,6
1State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, China. renqiang@cdut.edu.cn.
Nature communications
|January 3, 2025
概括
北中国区块 (North China Block) 是一个北中国区块.
科学领域:
- 古气候学 古气候学
- 古地质学 古地质学
- 构造学 构造学 构造学 构造学
背景情况:
- 追踪泰提斯海洋的潮湿干燥气候边界在石灰岩晚期到珀米亚早期是困难的.
- 了解全球干旱模式对于这个时期至关重要.
- 北中国区 (NCB) 经历了一种潮湿到干旱的气候转变在早期的波斯河.
研究的目的:
- 以NCB作为案例研究来追踪Tethys海洋的气候边界.
- 为了调查NCB在早期波斯纪期间干旱的驱动因素.
- 为了重建NCB的古地理位置.
主要方法:
- 北中国区块的古磁分析.
- 煤矿和红床沉积物的石化检查.
- 构造漂移与气候区过渡的相关性.
主要成果:
- 古磁数据显示,NCB在2.9亿至2.81亿年前迅速向北漂移.
- 这种变化使NCB从热带湿地转移到亚热带干旱地区.
- 从煤炭到红色床的石质变化与这种构造学和气候变化相关.
结论:
- 构造学漂移是早期波斯纪期间NCB干旱的主要驱动因素.
- 国家央行的漂移有助于划分泰提斯海洋的湿干界限.
- 这一发现与现代气候区分模式一致.
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