陕西石梯钡矿床中流体包裹体特征及成因意义  被引量:5

Characteristics of fluid inclusions in barite,witherite and barytocalcite from the Shiti barium deposit in southern Shaanxi and their genetic significance

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作  者:吴胜华[1,2] 刘家军[1,2] 柳振江[1,2] 翟德高[1,2] 要梅娟[1,2] 

机构地区:[1]中国地质大学地质过程与矿产资源国家重点实验室,北京100083 [2]中国地质大学地球科学与资源学院,北京100083

出  处:《中国地质》2010年第5期1469-1479,共11页Geology in China

基  金:国家自然科学基金(40573032);国家重点基础研究发展规划(2006CB403500);高等学校学科创新引智计划(B07011);长江学者和教育部创新团队发展计划项目资助

摘  要:陕西石梯重晶石-毒重石矿床产于南秦岭早古生代大型钡成矿带中。矿石类型有重晶石矿石、毒重石矿石、重晶石-毒重石混合矿石和钡解石矿石,但以重晶石矿石为主。经显微测温表明,重晶石中流体包裹体的均一温度范围为103.4~253.1℃(主峰值140~160℃),盐度范围为(0.35~10.73)wt%NaCleqv;毒重石中流体包裹体的均一温度范围为152.8~303.7℃(主峰值200~220℃),盐度范围为(0.18~9.73)wt%NaCleqv;钡解石中流体包裹体的均一温度范围为107.8~260.0℃(主峰值160~200℃),盐度范围为(0.71~8.41)wt%NaCleqv。经激光拉曼分析表明,在矿物流体包裹体的气相组成中,各矿物有一定差异:重晶石含一定量N2、H2S和CH4,毒重石含大量CO2和N2,而钡解石含有CO2、N2和CH4。成矿流体温度相对较高、富含CO2是形成毒重石的重要条件。The Shiti barite-witherite deposit of Shaanxi occurs in an early Paleozoic large Ba metallogenic belt of southern Qinling region.Barite,witherite,barite-witherite and barytocalcite constitute major ore types,with barite being the main ore.Microthermometry reveals that homogeneous temperatures and salinities of fluid inclusions in barite are from 103.4℃ to 253.1℃(main peak values 140~160℃) and from 0.35 wt%NaCl eqv.to 10.73wt%NaCl eqv.,homogeneous temperatures and salinities of fluid inclusions in witherite are from 152℃ to 303.7℃(main peak values 200~220℃) and from 0.18 wt%NaCl eqv.to 9.73wt%NaCl eqv.,and homogeneous temperatures and salinities of fluid inclusions in barytocalicite are from 107.8℃ to 260.0℃(main peak values 160~ 200℃) and from 0.71 wt%NaCl eqv to 8.41wt%NaCl eqv.,respectively.Laser Raman analyses show that gas phase compositions of fluid inclusions in these minerals are somewhat different:barite contains some N2,H2S and CH4,witherite contains abundant CO2 and N2,and barytocalicite contains some CO2,N2 and CH4.The relatively high temperature and abundant CO2 in fluids constitute conditions for witherite formation.

关 键 词:重晶石-毒重石矿床 流体包裹体 石梯 陕西 

分 类 号:P578.71[天文地球—矿物学]

 

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