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地质学报  2001 

中国季风沙区晚更新世以来环境及其变化

, PP. 127-137

Keywords: 中国季风区晚更新世-全新世湾地层剖面沙漠期气候波动季风沙区沉积环境

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Abstract:

本文以对毛乌素沙漠萨拉乌苏河流域米浪沟湾地层剖面晚更新世-全新世砂丘与河湖相、古土壤互为叠覆的高分辨率的气候地层记录的认识出发,同时基于对中国北方现代冬春季节风沙、尘霾活动发生的区域性气候-地质过程的理解,将今释古,反演了该时期中国季风区沙漠沙地曾经历的27个沙漠扩缩的周期性变化,并认为该剖面风砂沉积是过去地质时代季风沙区乃至整个中国沙区类似由现代这种冬春季西伯利亚-蒙古反气旋风系好冬季风向南伸展导致的若干风沙风尘动态过程的结果,而河湖相和古土壤的发育则主要与季风沙区受惠于东亚夏季风的影响有关。

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