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4 枪勇错沉积物饱和等温剩磁(SIRM, a)、特征样品2-2、2-12和2-19的IRM获得曲线的分解曲线(b~g)、一阶反转曲线(FORCs, h~j)和磁化率随温度变化(c-T, k~m)

Fig. 4 SIRM (a), Unmixing of IRM acquisition curves (b~g), FORCs (h~j) and c-T (k~m) of typical samples (2-2, 2-12 and 2-19) of Qiangyong Co Lake