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作 者:黄永高 冯佐海[1] 罗改 熊昌利[2] 张彤[2] 贾小川[2] 杨学俊[2] HUANG Yonggao;FENG Zuohai;LUO Gai;XIONG Changli;ZHANG Tong;JIA Xiaochuan;YANG Xuejun(Collaborative Innovation Center for Exploration of Hidden Noferrous Metal Deposits and Development of New Materials in Guangxi&School of Earth Science,Guilin University of Technology,Guilin,Guangxi 541004;Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province&Sichuan Geological Survey,Chengdu,Sichuan 610081)
机构地区:[1]桂林理工大学地球科学学院,广西有色金属隐伏矿床勘查及材料开发协同创新中心,广西桂林541004 [2]四川省地质调查院,稀有稀土战略资源评价与利用四川省重点实验室,四川成都610081
出 处:《地质与勘探》2020年第4期732-744,共13页Geology and Exploration
基 金:中国地质调查局项目(编号:DD20160016)资助。
摘 要:通甸地区地处三江特提斯兰坪盆地铅-锌-铜-银巨型矿集区东北部,具有寻找沉积岩型铅锌矿的前景。在通甸地区开展了1∶5万水系沉积物地球化学测量,以进一步指导铅锌矿勘察工作。确定了Pb、Zn和Ag等15种单元素异常范围,揭示了不同成因类型组合元素的分布特征及规律,圈定了21处地球化学综合异常。通过化探异常查证,识别出两条铅锌矿(化)体,经分析检测,Pb含量为1.93%~2.01%,Zn含量为0.48%~12.22%。研究表明,三合洞组(T 3 sh)碳酸盐岩和与其上下地层接触部位是区内重要的矿源层。结合异常分布规律、异常查证结果以及成矿地质背景进行综合评价,优选AS05甲1综合异常区为最佳铅锌找矿靶区,为通甸地区深入开展矿产勘查提供参考和依据。Tongdian area has good prospecting prospects for sediment-hosted lead-zinc deposits,which is situated in the northeast of the giant Pb-Zn-Ag-Cu ore-concentrated area of Lanping Basin,Sanjiang Tethys.To further assist in lead-zinc deposit prospecting,a 1∶50,000 stream sediment survey was carried out in this area.It delineated fifteen single element anomalies,including Pb,Zn,Ag,and defined twenty-one comprehensive geochemical anomalies.Also,it revealed the distribution characteristics and regularities of combined elements of different genetic types.According to verified geochemical anomalies,two lead-zinc ore-mineralized bodies(Pb of 1.93%~2.01%,Zn of 0.48%~12.22%)were identified.The study indicates that the Sanhedong Formation and its contact with the upper and lower strata are major source beds of lead-zinc deposits.Based on the anomaly verification,regularity of anomaly distribution,and geological setting of mineralization,the AS05-A 1 comprehensive anomaly was selected as the best lead-zinc prospecting target,which provides an important reference and basis for the geological prospecting in this area in the future.
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