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根据水质分析及古地理研究，作者认为兖州矿区岳庄水源地地下水中高含量硫酸盐主要是由于奥陶纪灰岩中含ＳＯ２－４的膏盐类矿物溶解产生的。
According to the analysis of water quality and palaeogeography, the author believes that the high content of sulphate in groundwater of Yuezhuang water source in Yanzhou Mining Area is mainly caused by dissolution of gypsum salt minerals containing SO2-4 in Ordovician limestone.