ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏龙玛拉铅锌矿床矽卡岩矿物特征及其地质意义
  
关键词:Tibet  skarn-type Pb-Zn deposits  Longmala  skarn zonation  skarn mineralogy
基金项目:中国地质调查局地质调查项目“芒康-江达一带铜多金属战略性矿产资源调查评价”(编号: DD20230361);国家自然科学基金项目(编号: 42002082);西藏中凯矿业股份有限公司勘查项目“西藏龙玛拉铅锌(铁)矿区成矿条件与找矿方向综合研究”(编号: HE2114)
作者单位E-mail
何逸飞 成都理工大学地球科学学院 742140610@qq.com 
谢富伟 成都理工大学地球科学学院 493743867@qq.com 
周敖日格勒 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  
王立强 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  
孙杨 成都理工大学地球科学学院  
张冠 西藏大学工学院  
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摘要:
Mineral Characteristics and Geological Significance of the Longmala Lead-zinc Skarn Deposit, Tibet
      The Longmala lead-zinc deposit is a typical skarn-type deposit located in the eastern section of Gangdese–Nyainqengtanglha lead-zinc metallogenic belt. Although the source and evolution of its ore-forming materials, diagenetic and metallogenic ages, and the dynamic background of its formation have been well studied, systematic research on its skarn mineralogy and zonation model is lacking. In this study, detailed field geological cataloging, systematic microscopic identification, and electron probe analysis were used to investigate the mineral association and composition as well as zonation characteristics of this skarn deposit in Tibet. Skarn minerals in the deposit mainly consist of garnet, pyroxene, wollastonite, chlorite, and epidote. The mineral association and chemical composition of the skarn have an obvious zonation in space. The skarn develops mainly in the contact zone between hornstone and marble or fills in the wall rock along cracks, showing transversal characteristics from faded hornstone → garnet skarn → dark hornstone → diopside skarn (ore body) → marble → hornstone. In the vertical direction from the roof to the floor, the lithological zonation is from hornstone → garnet skarn → diopside skarn → marble → garnet skarn → diopside skarn → hornstone. The garnet in the deposit belongs to the homomorphic series (And7.92~88.63Gro5.92~86.46Pyr+Spe1.04~5.11), with a wide range of end-member components, indicating that the environment in which the skarn formed is not a completely closed system. The garnet in the ore-bearing skarn of the main Pb-Zn ore body shows that the ore-forming fluid migrated from the southwest to the northeast to form the main ore body. These findings provide guidance for future searches for ore-forming rock masses and deep prospecting.
HE Yifei,XIE Fuwei,ZHOUAORI Gele,WANG Liqiang,SUN Yang,ZHANG Guan.2024.Mineral Characteristics and Geological Significance of the Longmala Lead-zinc Skarn Deposit, Tibet[J].Acta Geoscientica Sinica,45(2):175-188.
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