《Table 3 Major oxide (wt%) and trace element (ppm) concentration in the sediments of Urmia Salt Lake

《Table 3 Major oxide (wt%) and trace element (ppm) concentration in the sediments of Urmia Salt Lake   提示：宽带有限、当前游客访问压缩模式
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《"Mineralogy and Geochemistry of Major, Trace and Rare Earth Elements in Sediments of the Hypersaline Urmia Salt Lake, Iran"》


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Correlation coefficients of major elements（Table 2）show negative correlation between Al2O3 and Ca O（r=-0.96），which could be due to the inadequate feldspars or the Al2O3 introduced to the lake by river transportation.The positive correlation between Al2O3 and K2O（r=0.93）can be related to the presence of muscovite，illite and chlorite in the area.Positive correlation between Fe2O3with Ti O2（r=0.94）and Ti O2 with Mg O（r=0.63）in sediments might be due to the similar geochemical behavior in this environment and the mafic minerals such as hornblende and augite produced by mafic volcanic rocks and weathered gabbro intrusions in north of the lake.

图表编号XD0017175900    严禁用于非法目的
绘制时间2018.08.01
作者Samad ALIPOUR、Khadije MOSAVI ONLAGHI
绘制单位Geology Department, Faculty of Sciences, Urmia University、Urmia University
更多格式高清、无水印（增值服务）

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