[1]于守兵,李世杰,刘吉峰,等.青藏高原湖泊沉积研究及其进展[J].山地学报,2005,(06):663.
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青藏高原湖泊沉积研究及其进展()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2005年06期
页码:
663
栏目:
山地学报
出版日期:
2005-12-28

文章信息/Info

作者:
于守兵;李世杰;刘吉峰;
中国科学院南京地理与湖泊研究所;中国科学院南京地理与湖泊研究所;中国科学院南京地理与湖泊研究所 江苏南京210008;中国科学院研究生院;北京100039;江苏南京210008;江苏南京210008;中国科学院研究生院;北京100039
关键词:
青藏高原湖泊沉积研究进展
文献标志码:
A
摘要:
青藏高原湖泊沉积研究主要围绕青藏高原隆升和全球变化响应开展的。研究揭示了青藏高原隆升具有整体性、阶段性和后期加速性。中晚更新世以来和末次间冰期-冰期气候演化过程得到重建,并能够与冰芯和深海氧同位素记录对比;同时也存在MIS3阶段强烈暖湿和末次冰盛期冷湿等区域特征;新仙女木事件在湖泊沉积物也有明显记录。全新世研究表明青藏高原早期暖湿并经历冷事件,大暖期普遍出现高水位,后期气候向干冷化方向发展。湖泊沉积环境定量化重建也得到研究。青藏高原湖泊沉积应在高分辨率纹层沉积和环境指标定量分析基础理论方面加强研究。

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更新日期/Last Update: 2005-12-28