摘要
钡以BaSO_4形式存在的重晶石矿床在世界上广泛分布,但以BaCO_3形式存在的毒重石矿床极为罕见。在南秦岭早古生代硅岩建造中,发育大量层状毒重石和重晶石矿床,两类矿床在空间上表现出既共生又分离的分布规律,构成世界上极为独特的大型钡成矿带。本文对毒重石、钡解石、重晶石及石英等矿物流体包裹体进行了系统研究,结果显示,各矿物中流体包裹体的均一温度都变化于90～310℃,主要集中范围为120～220℃。尽管如此,毒重石、钡解石的形成温度峰值比重晶石高出40℃,而石英的形成温度分布较均一,没有出现明显的峰值。矿物流体包裹体的盐度虽变化于1%～15%NaCl_(eqv),但毒重石、钡解石和石英样品中的盐度值普遍大于5%NaCl_(eqv),而重晶石中的盐度值小于5%NaCl_(eqv)的样品数量占有相当大的比例。由于重晶石的流体包裹体主要以NaCl-H_2O型包裹体为主,而毒重石中富含大量N_2-CO_2-H_2S-CH_4等复杂组分水溶液型包裹体,显示出毒重石与重晶石在成矿环境上有较大差异。由此笔者明确提出,水溶液热化学硫酸盐还原作用是形成毒重石矿床主要机制的新认识。
The barite deposits in which Ba presents as BaSO4 are widespread in the world,whereas the witherite deposits in the presence of BaCO3 are rarely reported.Numerous layered witherite and barite deposits occur within the Early Paleozoic silicate formations of southern Qinling Mountains.These two types of deposits,representing a large-scale particular metallogenic belt in the world,exhibit paragenetic and separated distribution characteristics.This paper focuses on the fluid inclusion features of witherite,barytocalcite,barite,and quartz in the barium metallogenic belt.The results indicate that the homogenization temperature of fluid inclusions of each mineral ranges from 90 to 310℃,mainly concentrating at the range of 120-220℃.For all that,the peak of forming temperature of witherite and barytocalcite is higher than that of barite about 40℃,and quartz forming temperature distributes more homogeneously,and does not appear peak.The salinity of fluid inclusions of most minerals ranges from 1 to 15 wt%NaCl（eqv）,but the salinity of fluid inclusions of witherite,bary-tocalcite, and quartz generally is more than 5 wt%NaCl（eqv）,while for a considerable proportion of barite,the salinity of fluid inclusions is less than 5 wt%NaCl（eqv）.The fluid inclusions of the barite mainly are of NaCl-H2O type,whereas the fluid inclusions of witherite are rich in aqueous solution with complicated components like N2-CO2-H2S-CH4 etc.,which shows that there is a large difference between the metallogenic environments of witherite and barite.Based on these evidences,we suggest that the thermochemical sulfate reduction （TSR）of the solution was the main formation mechanism of witherite deposits.
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2010年第2期222-238,共17页
Earth Science Frontiers
基金
国家自然科学基金项目(40573032
40672067)
中国科学院地球化学研究所矿床地球化学国家重点实验室开放课题(0811)
国家重点基础研究发展计划"973"项目(2006CB403500
2009CB421003)
高等学校学科创新引智计划项目(B07011)
关键词
毒重石矿床
流体包裹体
热化学硫酸盐还原作用
南秦岭
witherite deposit
fluid inclusions
thermochemical sulfate reduction
southern Qinling
作者简介
作者简介：刘家军（1963-），男，教授，主要从事矿物学、岩石学、矿床学研究。E-mail：liujiajun@cugb．edu．cn
