PHYSICAL-CHEMICAL CONDITIONS FOR MINERALIZATION OF THE QINSHAN IRON DEPOSIT IN DATIAN COUNTY, FUJIAN PROVINCE
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摘要:
在野外地质工作基础上, 通过流体包裹体和氢氧同位素研究, 探讨福建大田琴山铁矿床形成的物理化学条件。流体包裹体研究显示, 均一温度均值355.6 ℃, 盐度(NaCl质量分数)均值4.4%, 流体密度均值0.65 g/cm3。流体演化成矿经历了400~420 ℃和240~280 ℃两个主要阶段, 其中400~420 ℃为晚矽卡岩阶段磁铁矿主要成矿温度, 形成深度约3 km, 该阶段以混合作用为主; 240~280 ℃为晚硫化物阶段铅锌矿主要成矿温度, 形成深度约1 km, 以沸腾作用为主。激光拉曼测试结果显示, 成矿流体含少量CH4和CO2。氢氧同位素显示, 早期成矿流体主要以岩浆水为主, 晚期成矿流体混入大量大气降水。研究结果表明琴山铁矿属于热液矽卡岩型矿床。
Abstract:Based on field investigation, the forming physical and chemical conditions of Qinshan iron deposit in Datian, Fujian were researched by fluid inclusions measurement and hydrogen and oxygen isotope. The homogenization temperature of fluid inclusions was 355.6 ℃, the salinity was 4.4%NaCl and the density was 0.65 g/cm3. Two peaks of homogenization temperature indicated that there were two stage of ore-fluid in the process of mineralization. The earlier stage was close related with the magnetite metallogenisis on the later skarn stage and the depth of about 3 km, the homogenization temperature was 400~420 ℃. The later stage was the Pb-Zn metallogenic stage and the depth of about 1 km, the fluid temperature was 240~280 ℃ and boiling. Raman analysis showed that the ore forming fluids contained little CO2 and CH4. The hydrogen and oxygen isotope data showed that the ore forming fluid mostly was derived from magma, and mixed with lot of meteoric water at later stage. Overall, the Qinshan Iron deposit was interpreted as a hydrothermal skarn deposit.
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表 1 流体包裹体显微测温结果
Table 1. Microthermometric data from fluids inclusions in the Qinshan iron deposi
样号(测点数) 样品类型 包裹体类型 充填度 均一温度/℃ 冰点温度/℃ 盐度/% 密度/(g·cm-3) 压力/MPa 深度/km 范围 均值 范围 均值 范围 均值 QSQ-3(2) 石榴子石-黄铁矿 Ⅰ 30 285~312 298.5 -0.1~-2.2 -1.1 0.18~3.71 1.94 0.74 8.30 0.83 QSQ-2(5) 石榴子石 50~70 386~402 395.3 -3.3~-6.8 -5.18 5.41~10.20 8.03 0.62 6.21 0.62 QPD3-1(8) 磁铁矿-石英脉 30~50 260~407 369.1 -0.1~-4.8 -3.74 0.18~7.59 6.05 0.65 19.90 1.99 QPD3-3(7) 磁铁矿-石英脉 20~40 239~343 270.1 -0.1~-1.8 -0.71 0.18~3.55 1.22 0.78 5.48 0.55 QPD3-4(8) 磁铁矿-石英脉 10~30 276~385 336.1 -0.1~-1.7 -0.63 0.18~2.90 1.08 0.77 5.72 0.57 QSQ-5(9) 黄铁矿-石英脉 20~31 185~248 231.7 -0.1~-3.7 -1.17 0.18~6.01 1.95 0.84 2.85 0.29 QPD2-1(5) 黄铁矿-石英脉 40~50 262~291 278.0 -0.7~-0.9 -0.80 1.22~1.57 1.40 0.84 6.18 0.62 QPD3-2(5) 石英脉 20~40 231~272 250.3 -0.3~-0.9 -0.55 0.53~1.57 0.96 0.81 3.97 0.40 QPD3-7(7) 石英脉 20~40 178~268 209.6 -2.4~-4.6 -3.36 4.03~7.31 5.47 0.90 1.83 0.18 QPD2-2(8) 石英脉-方铅矿-闪锌矿 20~30 140~320 248.5 -0.1~-1.5 -0.44 0.18~2.57 0.84 0.84 3.86 0.39 QSQ-1(3) 石榴子石 Ⅱ 50~60 398~427 412.0 -3.1~-5.9 -3.86 5.11~9.08 6.21 0.55 30.10 3.01 QSQ-4(4) 石榴子石-黄铁矿 20-30 401~470 432.9 -0.1~-11.5 -3.90 1.18~15.40 5.63 0.51 31.54 3.15 注：测试在南京大学内生金属矿床成矿机制研究国家重点实验室完成。WNaCl=0.00+1.78Tm-4.42×10-2Tm2+ 5.57×10-4 Tm3，Tm为冰点温度的绝对值(Hall等, 1988)；密度和最小压力参考NaCl-H2O流体体系估算[9] 
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表 2 氢、氧同位素组成
Table 2. Hydrogen and oxygen isotopic compositions from the Qinshan iron deposit
样品 产状 矿物 t/℃ δ18O石英/‰ δD流体/‰ δ18OH2O/‰ QPD2-1 石英-黄铁矿 石英 278 1.9 -54 -5.8 QPD2-2 石英脉-方铅矿-闪锌矿 石英 250 1.3 -51 -7.7 QPD3-1 磁铁矿-石英脉 石英 369 12.3 -53 7.5 QPD3-2 石英-黄铁矿 石英 270 4.1 -62 -4.0 QPD3-4 磁铁矿-石英脉 石英 336 10.4 -54 4.7 注：样品由中国地质科学院矿产资源研究所分析，计算采用的分馏方程为δ18O石英-δ18O水=1000lnα石英-水=3.38×106/T2-3.40[12]
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