首页|湘东北连云山上石地区伟晶岩型稀有金属矿床的发现及意义

湘东北连云山上石地区伟晶岩型稀有金属矿床的发现及意义

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湘东北地区位于钦杭成矿带中部北西缘,历来是中国重要的金、铜、钴、铅、锌多金属矿产区.在进行1∶10000地质填图过程中,在上石地区发现了大量锂辉石稀有金属矿脉,单样Li2O含量达到了 1.88%.其中包括:新发现伟晶岩脉25条,脉宽一米至数十米,延伸方向主要为北西西及近东西向,延伸数米至数百米;确定伟晶岩矿化点20余处,其中普遍发育锂辉石、铌钽铁矿、绿柱石等稀有金属矿物.伟晶岩脉与围岩存在明显的渐变分带,可细分为混合岩化片岩带(Ⅰ带)、二云母花岗岩带(Ⅱ带)、电气石伟晶岩带(Ⅲ带)和块状钠长石锂辉石带(Ⅳ带),各结构带之间分带明显.锂辉石多产于钠长石—锂辉石伟晶岩带中,伴生有大量巨晶电气石、白云母等,显示出良好的锂成矿潜力.同时大量伴生铌钽铁矿、绿柱石等稀有金属矿物,部分达到锂矿共伴生品位.矿床主要赋矿伟晶岩脉为近东西走向,长度超过1km,宽数米至数十米,厚度超过百米,Li2O平均品位为1.42%,初步预测储量约为2.56×104t,可达中型规模.该伟晶型锂稀有金属矿床的发现,彻底改变了湘东北地区以Be-Nb-Ta为主的稀有金属分布格局,暗示着区内稀有金属成矿的巨大潜力,对新一轮的找矿勘查具有启示意义.
Discovery and significance of pegmatitic rare metal deposits in Shangshi area,Lianyunshan,Northeast Hunan Province
The northeast of Hunan Province,located in the northwestern margin of the central part of the Qinzhou-Hangzhou metallogenic zone,has always been an important polymetallic metallogenic area of Au,Cu,Co,Pb and Zn in China.In this"Li-Co ore survey evaluation and target selection in Lianyunshan area of Hunan Province"project,we carried out the 1∶10 000 geological mapping process and found a large number of spodumene veins,whose single sample grade reached 1.78%.In addition,25 pegmatite veins were found,ranging from 1~10 meters in width,extending mainly in N-W and near E-W directions and from several meters to hundreds of meters.More than 20 mineralized spots of pegmatite were identified,including spodumene,niobium-tantalite,beryl and other rare metal minerals.There are obvious gradual zonings between pegmatite dike and surrounding rock,which can be subdivided into migmatite schist zone(Ⅰ),monzonite granite zone(Ⅱ),tourmaline pegmatite zone(Ⅲ)and massive albitite+spodumene zone(Ⅵ).The lithium ore bodies are mostly located in the massive albitite+spodumene zone,accompanied by a large number of giant crystal tourmaline,muscovite,etc.,showing good lithium metallogenic potential.A large number of rare minerals such as niobium-tantalite and beryl are associated,and some of which reach the co-associated grade of lithium ore.The main ore-bearing pegmatite vein of the deposit is near east-west trend,with a length of more than 1 km,a width of several meters to tens of meters,and a thickness of more than 100 meters.The average grade of Li2O is 1.42%,and the predicted reserves are about 2.56×104 t,which can reach medium scale.The discovery of pegmatitic lithium rare metal deposit in Shangshi area has completely changed the distribution pattern of rare metals dominated by Be-Nb-Ta,indicating the great potential of rare metal mineralization in this area,and of great guiding significance for the new round of ore exploration.

Rare metal depositZonation of pegmatiteLithium deposit of ShangshiLianyunshan areaNortheast of Hunan Province

文志林、黄明、许国锋、张云飞、黄宝亮、李荫中、刘磊

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湖南省地质灾害调查监测所 长沙 410014

中南大学有色金属成矿预测与地质环境监测教育部重点实验室 长沙 410083

中南大学地球科学与信息物理学院 长沙 410083

稀有金属矿床 伟晶岩分带 上石锂矿床 连云山地区 湘东北

国家自然科学基金面上项目湖南省省级财政地质勘查项目湖南省自然科学基金面上项目江南陆块南缘成矿带(东段)战略性矿产调查项目

4197219820240032022JJ30702DD20240066

2024

地质科学
中国科学院地质与地球物理研究所

地质科学

CSTPCD北大核心
影响因子:0.79
ISSN:0563-5020
年,卷(期):2024.59(4)
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