粤北仁化棉花坑铀矿床地下热水地球化学特征及补给来源研究
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摘要
通过对粤北仁化棉花坑铀矿床地下热水的水文地球化学及地热地质条件分析,探讨了地下热水的形成环境及补给源特征。棉花坑矿床地下热水为HCO_3~--Ca~(2+)-Na~+型水,其δD_(V-SMOW)值为-44.5‰～-40.7‰,δ~(18)O_(V-SMOW)值为-6.8‰～-6.4‰,分布于本地雨水线附近,为大气降水成因;热储温度为67.8℃,补给源高程为650～1150 m,循环深度为标高-1250～-660 m,d-excess值7.5‰～10.5‰,表明地下热水可更新能力较强,热水径流距离短,水—岩作用较弱;结合粤北花岗岩区地质地貌特征,认为补给源来自矿床东南向的南山一带;地下水深循环是形成矿区地热主因,同时岩体铀矿物放射性蜕变产热可增强地温梯度;地下热水铀含量为40～120μg/L,呈氧化环境,现今地下热水活动一定程度上继承了成矿期古热水活动特征,对铀矿床的形成具有促进作用;热水循环深度指示矿床深部仍具有非常好的找矿前景。
Objectives:The paper has discussed the formation environment and recharge source of geothermal water,based on the analysis of hydrogeochemical and geological conditions in the Mianhuakeng Uranium Deposit,Northern Guangdong.Methods:This paper was based on the methods of hydrochemical analysis,H—O isotope analysis and comprehensive study of water samples.Results:The geothermal water type was HCO_3~-—Ca~(2+)—Na~+,andδD_(V-SMOW)ranged-44.5‰～-40.7‰,δ~(18)O_(V-SMOW)ranged-6.8‰～-6.4‰,distributed near the local rainwater line which was caused by atmospheric precipitation.The water had strong renewability,short runoff distance and weak water—rock effect,which thermalstorage temperature was 67.8℃,recharge source altitude 650～1150 m,circulation depth altitude-1250～-660 m,and d-excess value ranged 7.5‰～10.5‰The uranium content which was 40～120μg/L indicated that the geothermal water was formed in an oxidizing environment.Conclusions:The recharge source was come from Nanshan area which was located in southeast of the deposit,according to the geological and geomorphologic characteristics of granite area in northern Guangdong.The groundwater depth recycle was the main reason of geothermal formation.To some extent,the present geothermal water activity has inherited the characteristics of the paleo hot water during the metallogenic period,which had a promoting effect on the formation of uranium deposit.The depth recycle of the geothermal water has indicated that there was a very good prospecting potential in the depth of the deposit.
Objectives:The paper has discussed the formation environment and recharge source of geothermal water,based on the analysis of hydrogeochemical and geological conditions in the Mianhuakeng Uranium Deposit,Northern Guangdong.Methods:This paper was based on the methods of hydrochemical analysis,H—O isotope analysis and comprehensive study of water samples.Results:The geothermal water type was HCO_3~-—Ca~(2+)—Na~+,andδD_(V-SMOW)ranged-44.5‰～-40.7‰,δ~(18)O_(V-SMOW)ranged-6.8‰～-6.4‰,distributed near the local rainwater line which was caused by atmospheric precipitation.The water had strong renewability,short runoff distance and weak water—rock effect,which thermalstorage temperature was 67.8℃,recharge source altitude 650～1150 m,circulation depth altitude-1250～-660 m,and d-excess value ranged 7.5‰～10.5‰The uranium content which was 40～120μg/L indicated that the geothermal water was formed in an oxidizing environment.Conclusions:The recharge source was come from Nanshan area which was located in southeast of the deposit,according to the geological and geomorphologic characteristics of granite area in northern Guangdong.The groundwater depth recycle was the main reason of geothermal formation.To some extent,the present geothermal water activity has inherited the characteristics of the paleo hot water during the metallogenic period,which had a promoting effect on the formation of uranium deposit.The depth recycle of the geothermal water has indicated that there was a very good prospecting potential in the depth of the deposit.
引文
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