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8 冷水坑矿床下鲍矿段132号勘探线剖面略图[9] 1—下白垩统鹅湖岭组;2—下白垩统打鼓顶组;3—震旦系老虎塘组;4—花岗斑岩;5—流纹斑岩;6—层状铅锌银矿体;7—斑岩型矿体;8—推测断层

Fig.8 Profile of No.132 exploration line in Xiabao ore block of Lengshuikeng deposit[9] 1—lower Cretaceous Ehuling formation; 2—lower Cretaceous Daguding formation; 3—Sinian Laohutang formation; 4—granite porphyry; 5—rhyolitic porphyry; 6—layered lead zinc silver ore body; 7—porphyry ore body; 8—inferred fault