相山矿田与冷水坑矿田多金属成矿特征对比

庞文静, 陈贝贝, 周涛, 黄柔睿, 周云云, 郭福生, 吴志春, 谢财富

A comparative study on polymetallic metallogenic characteristics of Xiangshan and Lengshuikeng ore fields

PANG Wen-Jing, CHEN Bei-Bei, ZHOU Tao, HUANG Rou-Rui, ZHOU Yun-Yun, GUO Fu-Sheng, WU Zhi-Chun, XIE Cai-Fu

图7 相山矿田牛头山地区26线剖面 1—下白垩统鹅湖岭组上段;2—下白垩统打鼓顶组上段;3—下白垩统打鼓顶组下段;4—中元古界;5—施工的钻孔;6—多金属蚀变范围;7—多金属矿体

Fig.7 Profile of line 26 in Niutoushan area of Xiangshan ore field 1—upper part of the lower Cretaceous Ehuling formation; 2—upper part of the lower Cretaceous Daguding formation ; 3—lower part of the lower Cretaceous Daguding formation; 4— Mesoproterozoic; 5—drilling for construction; 6—polymetallic alteration range; 7—polymetallic ore body