CAJ | 학술논문

广西平南县平村半隐伏花岗岩岩体侵入于寒武系黄洞口组地层，其西南大部分被泥盆系莲花山组地层所覆盖。该半隐伏岩体以隐爆角砾岩小岩株为露头，在寒武系地层中发育密集的花岗斑岩脉。其剥蚀程度浅，成矿条件好，但地质工作程度低。分析认为在其出露范围内新发现的罗平钨矿具有大型、超大型钨矿床规模的找矿潜力。该半隐伏岩体与钨矿成因上的密切关系对大瑶山成矿带今后的找矿工作具有深远的指导意义。
엄서평남현평촌반은복화강암암체침입우한무계황동구조지층，기서남대부분피니분계연화산조지층소복개。해반은복암체이은폭각력암소암주위로두，재한무계지층중발육밀집적화강반암맥。기박식정도천，성광조건호，단지질공작정도저。분석인위재기출로범위내신발현적라평오광구유대형、초대형오광상규모적조광잠력。해반은복암체여오광성인상적밀절관계대대요산성광대금후적조광공작구유심원적지도의의。
Pingcun semi-concealed granite rock mass of Pingnan in Guangxi intrudes into the strata of Cambri-an Huangdongkou Formation,and most of its southwestern part is covered by the strata of Devonian Lian-huashan Formation.The semi-concealed rock mass outcrops as small stocks of cryptoexplosion breccia and develops dense granite dikes in Cambrian strata.This area is characterized by superficial denudation,favora-ble metallogenic conditions and lack of completed geological works.Through analysis,the author believes that it is possible to find a large or super-large scale tungsten deposit in the newly discovered Luoping W de-posit which is located inside the range of the outcrops.This semi-concealed rock mass has close genetic rela-tionship with tungsten deposit,and it has significance in guiding future prospecting works in Dayaoshan met-allogenic belt.