1899—2011年青藏高原南部枪勇错沉积物磁性矿物的环境意义

高星, 康世昌, 刘青松, 陈鹏飞, 段宗奇

Magnetic characteristics of Qiangyong Co Lake sediments, southern Tibetan Plateau and its environmental significance during 1899-2011

GAO Xing, KANG Shichang, LIU Qingsong, CHEN Pengfei, DUAN Zongqi

图7 枪勇错磁性矿物不同组分的占比变化(a~d)与浪卡子气象站降水(e)、气温(f)、青藏高原平均气温变化、北半球平均温度变化(g)和Hg含量的变化趋势 注：Hg含量变化及年代数据来自文献[12];青藏高原和北半球平均温度距平数据来自文献[16]。

Fig. 7 The variations of different magnetic components of Qiangyong Co Lake (a~d), annual precipitation (e) and average temperature (f) from Nargaze station, temperature anomaly of the Tibetan Plateau and the Northern Hemisphere (g), and Hg content (h)