ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏多龙矿集区铁格隆南铜(金)矿床黄铁矿特征及意义
  
关键词:Tibet  Tiegelongnan porphyry-epithermal deposit  pyrite  element geochemistry  S isotope
基金项目:国家重点研发计划项目“西藏铜多金属资源基地绿色勘查与增储示范”(编号: 2022YFC2905001);国家自然科学基金项目(编号: 42002103);中国地质调查局地质调查项目“铜(金)锑等紧缺战略性矿产调查与潜力评价”(编号: DD20230054)
作者单位E-mail
张琪 中国地质大学(北京)地球科学与资源学院 HanZQ497@outlook.com 
陈伟 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室 nmgchenwei@163.com 
杨欢欢 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
付雪莲 成都理工大学地球科学学院  
王勤 成都理工大学地球科学学院  
李彦波 西藏自治区地质矿产勘查开发局第五地质大队  
李宏伟 西藏自治区地质矿产勘查开发局第五地质大队  
辛堂 西藏自治区地质矿产勘查开发局第五地质大队  
梁鑫娟 成都理工大学地球科学学院  
李社 中铝西藏金龙矿业股份有限公司  
刘长城 中铝西藏金龙矿业股份有限公司  
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摘要:
Characteristic and Significance of Pyrite at Tiegelongnan Cu (Au) Deposit, Duolong Ore District, Tibet
      The Tiegelongnan porphyry-epithermal Cu (Au) deposit is one of the most important deposits in the Bangongco–Nujiang metallogenic belt, where pyrite is extensively developed. In this study, trace elements, rare earth elements (REE), and S isotopes of pyrite were analyzed. Three types of pyrite were identified according to their occurrence characteristics: pyrite-1 and pyrite-2 were related to epithermal mineralization, and pyrite-3 was related to porphyry mineralization. Pyrite-1 had the lowest Au, Ag, Cu, Pb, Zn, and Bi concentrations, whereas pyrite-2 had the highest Au, Ag, Cu, Pb, Zn, and Bi concentrations. The correlations between Cu and Ni, Ag and Cu, Cu and Pb, Ag and Pb, and Pb and Zn could be used to distinguish pyrite-2 from pyrite-3. The δ34S value for pyrite-1 (1.9‰) was the highest among the three types. The δ34S values for pyrite-2 and pyrite-3 were between –4.5‰ and 0.3‰, respectively. Pyrite was rich in LREE and depleted HREE and hada “right tilt” pattern in REE distribution. The REE differentiation of pyrite in the shallow deposits (200–450 m) was relatively large with a positive Eu anomaly, whereas the REE differentiation of pyrite in deeper deposits (700–1000 m) was small with a negative Eu anomaly. The migration direction of the sulfur-containing hydrothermal solution in the Tiegelongnan deposit was horizontal from ZK1604 towards the East and vertical from 230–250 m at ZK1604 to the deep and lateral. The high concentrations of Cu, Au, and Ag in pyrite and the positive correlations between Ag and Cu, Pb and Zn, Cu and Pb, and Ag and Pb were important indicators of epithermal mineralization, whereas the negative correlation between Cu and Ni in pyrite indicated porphyry mineralization.
ZHANG Qi,CHEN Wei,YANG Huan-huan,FU Xue-lian,WANG Qin,LI Yan-bo,LI Hong-wei,XIN Tang,LIANG Xin-juan,LI She,LIU Chang-cheng.2023.Characteristic and Significance of Pyrite at Tiegelongnan Cu (Au) Deposit, Duolong Ore District, Tibet[J].Acta Geoscientica Sinica,44(6):983-999.
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