萨拉乌苏河流域干沟子剖面全新世湖相沉积的地球化学元素特征及其反映的物源变化
周维鑫, 温小浩, 李保生, 王晨, 田梦圆, 邱明昆

Geochemical characteristics of holocene lacustrine sediments in Gangouzi section and its sedimentary sources in the Salawusu River Valley
Weixin Zhou, Xiaohao Wen, Baosheng Li, Chen Wang, Mengyuan Tian, Mingqun Qiu
表2 干沟子剖面常量元素氧化物含量分布(%
Table 2 Content distribution of major element oxides in Gangouzi section %
沉积层段数值类型SiO2CaOAl2O3MgOTFeNa2OK2OTiO2
0—110 cm最大值93.5229.9310.066.231.502.632.100.29
最小值30.540.874.500.463.900.830.910.12
平均值44.0618.677.043.622.261.581.430.19
110—250 cm最大值89.571.0511.021.233.902.632.560.29
最小值68.580.726.840.140.701.432.020.16
平均值77.900.839.470.671.991.642.270.22
全剖面最大值93.5229.9311.026.233.902.632.560.30
最小值30.540.724.500.140.700.830.910.13
平均值60.849.828.242.152.121.611.840.20
标准偏差19.2110.121.661.860.680.390.480.04
变异系数0.321.030.200.870.320.240.260.20