• 责任者：Yang Liu (School of Geosciences and Info-Physics ; Central South University ; Changsha 410083 ; China) ; Zou Haiyang
• 刊名：Geology and Prospecting
• 出版年：2012
• 卷期：50(4)
• 关键词：金矿 ; gold ores ; 山东 ; Shandong Province
• 页码：p.677-684
• 图表：3 illus., 3 tables, 18 refs.
• 分类号：1001
• issnNo：ISSN0495-5331
• isbnNo：CN11-2043/P

 This paper 0analyzed the fluid inclusions,micro-thermometry and rare earth elements of the Jinchiling gold deposit in Shandong Province.The objective was to study the property and evolution of the ore-forming fluid of this gold deposit.The result shows that these inclusions are dominated by gas and liquid two-phase ones,with few of liquid phase.The compositions of gas in the inclusions are primarily H2O and CO2.The liquid composition is Na+-K+-Ca2+-Mg2+-Cl--SO2-4,and ore-forming fluid is the mixed fluid of magmatic hydrothermal and meteoric water.The homogenization temperature is 140℃～350℃.The main mineralization of gold occurred in the second and third stages of the evolution when the temperature was 185℃～290℃.And the salinity of fluid inclusions is 7.3% to 8.9%,implying an ore-formation fluid of intermediate-low temperature and low salinity.The REE(rare earth element) analysis shows that the inclusions are characterized by LREE(light rare earth element) enrichment,HREE(heavy rare earth element) deplerion,middle negative Eu anomalies,and slightly right-deviation standardization curves.