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山东金岭铁矿属接触交代型矿床.沿金岭闪长杂岩体与中奥陶统马家沟组灰岩、中石炭统本溪组砂、页岩的接触带上分布有肖庄、侯庄、铁山、北坑、北金召、东召口、王旺庄等多个大小不等的矽卡岩矿床.通过对分布于中奥陶统马家沟组灰岩中膏盐、硫化物、矿体和矽卡岩、岩体赋存的硫酸盐、硫化物进行δS~(34)的分析,获得了金岭闪长岩体的硫同位素组成δS~(34)=-0.4～14.6‰,δS~(34)的众值范围:4.3～9.8‰,沉积围岩的δS~(34)=-1.4～18.1‰,δS~(34)的众值范围:7.2
The Jinling iron ore belongs to the contact metasedimentary deposit, along the contact zone between the Jinling diorite complex and the Middle Ordovician Majiagou limestone, the Carboniferous Benxi formation sand and the shale, Xiaozhuang and Hou Zhuang, Tieshan, Beikeng, Beijinzhao, Dongzhaokou, Wangwangzhuang and other sizes of skarn deposits.According to the distribution of limestone in the Middle Ordovician Majiagou limestone, sulfide The δS ~ (34) of sulphides and sulfides from the rock mass was used to analyze the sulfur isotopic composition of the Jinling diorite body, δS ~ (34) = -0.4 ~ 14.6 ‰, the range of δS ~ (34): 4.3 ~ 9.8 ‰, δS ~ (34) = 1.4 ~ 18.1 ‰, δS ~ (34)