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3 冷水坑矿田地质图[9] 1—第四系;2—下白垩统鹅湖岭组;3—下白垩统打鼓顶组;4—石炭系梓山组;5—上震旦统老虎塘组;6—流纹斑岩;7—钾长花岗斑岩;8—石英正长斑岩;9—含矿花岗斑岩;10—隐爆角砾岩;11—不整合界线;12—断层;13—勘探线

Fig.3 The geological map of Lengshuikeng ore field[9] 1—Quaternary; 2—lower Cretaceous Ehuling formation; 3—lower Cretaceous Daguding formation; 4—Carboniferous Zishan formation; 5—upper Sinian Laohutang formation; 6—rhyolitic porphyry; 7—K-feldspar granite porphyry; 8—quartz syenite porphyry; 9—ore bearing granite porphyry; 10—cryptoexplosive breccia; 11—unconformity boundary; 12—fault; 13—exploration line