CAJ | 학술논문

利用红外显微镜对湖南瑶岗仙石英脉型黑钨矿矿床中共生的黑钨矿与石英原生流体包裹体均一温度和冰点的测定结果表明,石英中流体包裹体均一温度范围为149～352℃,主要集中在160～300℃之间,盐度w(NaCl_(eq))为0.9%～9.5%;黑钨矿中流体包裹体均一温度范围为212～386℃,主要集中在280～360℃之间,盐度w(NaCl_(eq))为4.5%～15.2%.可见,黑钨矿中流体包裹体具有更高的均一温度和盐度,与石英中原生流体包裹体均一温度相差可达60℃,盐度w(NaCl_(eq))相差可达6%.结合该矿床的矿石显微结构特征、包裹体岩相学特征及前人所做的氢、氧同位素测试分析结果,推断黑钨矿主要形成于早期阶段,为均一流体冷却成因,石英形成较晚,主要为流体混合成因.
이용홍외현미경대호남요강선석영맥형흑오광광상중공생적흑오광여석영원생류체포과체균일온도화빙점적측정결과표명,석영중류체포과체균일온도범위위149～352℃,주요집중재160～300℃지간,염도w(NaCl_(eq))위0.9%～9.5%;흑오광중류체포과체균일온도범위위212～386℃,주요집중재280～360℃지간,염도w(NaCl_(eq))위4.5%～15.2%.가견,흑오광중류체포과체구유경고적균일온도화염도,여석영중원생류체포과체균일온도상차가체60℃,염도w(NaCl_(eq))상차가체6%.결합해광상적광석현미결구특정、포과체암상학특정급전인소주적경、양동위소측시분석결과,추단흑오광주요형성우조기계단,위균일류체냉각성인,석영형성교만,주요위류체혼합성인.
In order to understand the differences between the fluid inclusions in ore minerals and those in gangue mine-rals, the authors performed a microthermometric study of fluid inclusions in wolframite and coexisting quartz from the Yaogangxian quartz-vein wolframite deposit by using infrared microscopy. The results show that homo-geneous temperature (t_h) and salinity of fluid inclusions in quartz are obviously different from those in wol-framite, in spite of the fact that these two minerals were formed at the same ore-forming stage. The data show that the homogeneous temperatures of fluid inclusions in quartz are 149 ～ 352℃, mainly concentrated in the range of 160～300℃, and the salinities are 0.9%～9.5% ; whereas the homogeneous temperatures of fluid in-elnsions in wolframite are 212 ～ 386℃, concentrated at 280 ～ 360℃, and the salinities are 4.5 % ～ 15.2%.Thus, the fluid inclusions in the quartz have lower homogeneous temperature and salinity than those in wol-framite. The differences of homogeneous temperatures between wolframite and quartz can reach 60℃ and those of salinities can reach 6 %. Combined with H, O isotope analyses and ore micro-texture features, the authors have drawn a conclusion that the fluids captured in wolframite were formed at an early stage when the solution was homogeneous, and the temperature declining was the main cause for mineral deposition, whereas the fluids in quartz had mixed fluid properties of igneous fluid and underground water, suggesting their formation at a later stage.