ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
长坑金银矿床的铅,锶,硫同位素特征与矿化模式
  
关键词:isotopes of lead and sulfur  anomalous lead of multi-stage  fluid mixing gold silver deposit  Changkeng
基金项目:中国科学院黄金办科研基金,中科院博士点基金
作者单位
张生 中国科学院广州地球化学研究所 
李统锦 中国科学院广州地球化学研究所 
王联魁 中国科学院广州地球化学研究所 
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摘要:
Characteristics of Lead, Strontium and Sulfur Isotopes and Mineralization Model of Changkeng Gold Silver Deposit, China
      The isotopic composition of lead of gold ore is somewhat different from silver ore in Changkeng deposit, i.e., the variation of 206 Pb/ 204 Pb of gold ore is vider while silver ore enrichs 207 Pb and 208 Pb relatively. The lead of gold ore belongs to anomalous lead derived from mixing of common lead with radiogenic lead, and the lead of silver ore probably represents mixture of lead isotopes having undergone three stage evolution. The lead isotope, as well as strontium isotope of calcite, is of crust origin, The δ 34 S values of gold ore are scattered with negative average, while silver ore relatively gathered with positive average. Based on the correlation betwween sulfur and lead isotopic compositions and the zoning of gold and silver ores, a mineralization model for mixing process of fluids with different lead isotopic compositions and oxidizing potentials is presented for Changkeng deposit in this paper.
ZHANG Sheng,LI Tong-jin,WANG Lian-kui.1997.Characteristics of Lead, Strontium and Sulfur Isotopes and Mineralization Model of Changkeng Gold Silver Deposit, China[J].Acta Geoscientica Sinica,18(1):53-60.
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