塔克利马坎沙漠的年龄
1State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Post Office Box 9825, Beijing 100029, China. jmsun@mail.igcas.ac.cn
概括
塔克利马坎沙漠在530多万年前由于气候变化和西藏高原升高而形成. 这导致了塔林盆地广泛的沙丘,风吹的泥沉积物证明了这一点.
科学领域:
- 地质地质地质地质地质地
- 古气候学 古气候学
- 构造学 构造学 构造学 构造学
背景情况:
- 塔克利马坎沙漠位于塔里姆盆地,这是一个与西藏高原相邻的草原盆地.
- 了解沙漠的形成对于重建区域环境和构造历史至关重要.
研究的目的:
- 为了研究南方塔克利马坎沙漠的平流图序列.
- 为了确定塔林盆地荒漠化的时间和原因.
主要方法:
- 一个1626米厚的沉积物序列的平流图分析.
- 识别和解释交叠的风吹泥层.
主要成果:
- 证据表明,塔林盆地至少在530万年前就出现了移动沙丘的流行.
- 在研究的部分积聚的岩泥直接与沙漠的形成和扩张有关.
- 这些发现与代晚期的气候恶化和大气循环模式的变化相关.
结论:
- 塔克利马坎沙漠的形成至少开始于530万年前.
- 西藏高原的升起和相关的气候变化是塔林盆地荒漠化的主要驱动因素.
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