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新疆萨喀尔得铜矿C-H-O-S同位素特征
引用本文:吕兵团,王先林,石满乾,王利鹏,柳志进.新疆萨喀尔得铜矿C-H-O-S同位素特征[J].中国区域地质,2014(1):104-109.
作者姓名:吕兵团  王先林  石满乾  王利鹏  柳志进
作者单位:[1]长安大学/地球科学与国土资源学院,陕西西安710064 [2]中国人民武装警察部队黄金第七支队,山东烟台264004
基金项目:中国地质调查局项目(编号:1212011120495、1212011220661)致谢:成文过程中石家庄经济学院牛树银教授和审稿人提出了宝贵的修改意见和建议,在此表示诚挚的谢意.
摘    要:新疆萨喀尔得铜矿属中低温热液型,该矿石英和方解石样品中^δ13CPDB值为-17.3‰— -0.7%,δ^18OSMOW为16.2‰-22.4‰ δ18OH2O 水值为6.9‰-12.5‰水值为6.9‰-12.5‰,8D变化于-73.8‰—-52.4‰之间。研究表明,成矿流体主要来源于深部发生循环加热的建造水,并混合变质水和岩浆水;成矿早期流体中的C主要来源于地层水或大气降水,晚期有深部岩浆水的加入。^δ^34S值变化范围为0.2‰-6.1%o,表明流体中的S主要来自岩浆或上地幔。

关 键 词:C—H-O-S同位素  成矿流体  萨喀尔得铜矿  新疆

The C-H-O-S isotope characteristics of the Sakaerde copper deposit in Xinjiang.
LU Bing-tuan,WANG Xian-lin,SHI Man-qian,WANG Li-peng,LIU Zhi-jin.The C-H-O-S isotope characteristics of the Sakaerde copper deposit in Xinjiang.[J].Regional Geology of China,2014(1):104-109.
Authors:LU Bing-tuan  WANG Xian-lin  SHI Man-qian  WANG Li-peng  LIU Zhi-jin
Institution:1. Faculty of Earth Sciences and Land Resource, Chang'an University, Xi'an 710064, Shaanxi, China; 2. The 7th Gold Detachment of Chinese Armed Police Force, Yantai 264004, Shandong, China
Abstract:The Sakaerde copper deposit is a mesothermal-epithermal deposit. The 8 I~CPDB values of quartz and calcite samples in the deposit vary in a narrow range of- 17.3%0~-0.7%0. The ~ ~8OsMow values range from 16.2‰ to 22.4‰, their corresponding ^18OH1O values are between 6.9%0 and 12.5‰, and the 8 D values of fluid inclusions vary from -73.8‰ to -52.4‰. These data imply that the ore-forming fluids of the ore deposit were mainly derived from the heated formation water mixed with a small amount of magmatic water and metamorphic water. The carbon in ore-forming fluids mainly came from formation water or atmosphere precipi- tation, with the addition of some deep magmatic water at the late stage. The δ^34S values range from 0.2‰to 6.1‰, implying that the sulfur in ore fluids mainly came from the magma or the upper mantle.
Keywords:C-H-O-S isotope  ore-forming fluid  Sakaerde copper deposit  Xinjiang
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