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2 相山矿田地质图[8] 1—第四系;2—上白垩统南雄组; 3—下白垩统鹅湖岭组上段;4—下白垩统鹅湖岭组下段;5—下白垩统打鼓顶组上段;6—下白垩统打鼓顶组下段;7—三叠系安源组; 8—石炭系华山岭组;9—中元古界;10—花岗斑岩; 11—花岗岩;12—断裂构造

Fig.2 The geological map of Xiangshan ore field[8] 1—Quaternary; 2—upper Cretaceous Nanxiong formation; 3—upper part of the lower Cretaceous Ehuling formation; 4—lower part of the lower Cretaceous Ehuling formation; 5—upper part of the lower Cretaceous Daguding formation; 6—lower part of the lower Cretaceous Daguding formation; 7—Triassic Anyuan formation; 8—Carboniferous Huashanling formation; 9— Mesoproterozoic; 10—granite porphyry; 11—granite; 12—fault structure