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江西宜丰水南矿区花岗岩型锂矿床地质特征及成因分析

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九岭南缘宜丰—奉新地区发育巨量花岗岩型锂矿,锂矿主要赋存于燕山期花岗岩,成矿类型为花岗岩锂云母型,水南矿区是其中典型矿床之一.以水南矿区花岗岩型锂矿为研究对象,在系统收集野外资料的基础上,总结矿床地质特征;结合矿床蚀变特征、锂的赋存状态,分析花岗岩型锂矿床成因.研究表明:锂矿体赋存于燕山期白水洞岩体白云母(二长)花岗岩中,锂主要赋存于锂云母、铁锂云母和富锂白云母等矿物中.矿区含矿岩体为高演化过的铝质花岗岩,岩浆演化程度越高,岩体越富锂,岩浆的结晶分异导致锂等成矿元素在残余熔体中不断富集;除结晶分异作用,白云母花岗岩中富锂云母的核边结构显示出热液蚀变特征,锂元素由于独特的化学性质,导致他优先富集于花岗质岩浆或岩浆热液中,后期富锂热液对白云母强烈改造交代,使得成矿元素在云母边界形成高度富集的锂云母.因此矿区锂矿成因兼具岩浆分异和热液蚀变特征.
Geological Characteristics and Genesis Analysis of Granite-type Lithium Deposit in Shuinan Mining Area,Yifeng,Jiangxi
A large number of granite-type lithium deposits are developed in the Yifeng-Fengxin area on the southern margin of the Jiuling Mountains.Lithium deposits are mainly hosted in Yanshanian granites.The metallogenic type is granite lithium mica-type lithium deposits.Shuinan mining area is one of the typi-cal deposits.Taking the lithium deposits in the Shuinan mining area as research object,based on the system-atic collection of field data,the geological characteristics of the deposit are summarized,and the genesis of granite-type lithium deposits is analyzed in combination with the alteration characteristics of the deposit and the occurrence state of lithium.The results show that the lithium ore body occurs in muscovite(monzonitic)granite of Baishuidong rock mass in Yanshan period,and lithium mainly occurs in minerals such as lepido-lite,iron lithium mica and lithium rich muscovite.The ore-bearing rock mass is highly evolved peralumi-nous granite.The higher the degree of magmatic evolution,the more lithium-rich the rock mass.The crystal-lization differentiation of the magma leads to the continuous enrichment of lithium and other ore-forming ele-ments in the residual melt.In addition to crystallization differentiation,the core-rim structure of lithium-rich mica in muscovite granite shows hydrothermal alteration characteristics.Lithium is preferentially en-riched in granitic magma or magmatic hydrothermal solution due to its unique chemical properties.In the lat-er stage,the lithium-rich hydrothermal fluid strongly reformed the muscovite,making the ore-forming ele-ments form a highly enriched lepidolite at the mica boundary.Therefore,the genesis of lithium deposits in the mining area has both magmatic differentiation and hydrothermal alteration characteristics.

Granite type lithium oregeological characteristics of depositore genesis

赖长金、马超、吴远亮、李箭箭

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江西省找矿突破勘查技术中心

江西省地质局第一地质大队

花岗岩型锂矿 矿床地质特征 矿床成因

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(12)