CAJ | 학술논문

江西南部金华寺测区位于南岭成矿带与武夷山隆起成矿带结合部位，属南武夷锰－锡－铜－金－银－铅－锌成矿亚带。在1∶2．5万沟系沉积物测量的基础上，选取异常较好地段进行1∶1万土壤地球化学测量，分析元素地球化学特征。针对测区内土壤地球化学元素异常较好地段进行岩石地球化学分析，进一步剖析其含矿性。结合野外地质调查，初步总结了测区内主要成矿元素的地球化学勘查模型及找矿方向。研究表明，金华寺测区 Ag、Au 地球化学异常明显，与断裂活动、辉绿岩脉关系密切；异常区具有一定的矿化，其中1号 Ag 异常地表矿化好，但深部找矿潜力有待查明。
강서남부금화사측구위우남령성광대여무이산륭기성광대결합부위，속남무이맹－석－동－금－은－연－자성광아대。재1∶2．5만구계침적물측량적기출상，선취이상교호지단진행1∶1만토양지구화학측량，분석원소지구화학특정。침대측구내토양지구화학원소이상교호지단진행암석지구화학분석，진일보부석기함광성。결합야외지질조사，초보총결료측구내주요성광원소적지구화학감사모형급조광방향。연구표명，금화사측구 Ag、Au 지구화학이상명현，여단렬활동、휘록암맥관계밀절；이상구구유일정적광화，기중1호 Ag 이상지표광화호，단심부조광잠력유대사명。
Located at the junction of the Nanling metallogenic belt and the Wuyishan metallogenic belt, Jinhuasi surveyed area in southern Jiangxi belongs to the South Wuyi manganese?tin?copper?gold?silver?lead?zinc metallogenic subzone. On the basis of 1 ∶ 25, 000 gully sediments survey, the good anomalous segments were selected to conduct 1 ∶ 10,000 soil geochemical survey for analyzing el?ement geochemical characteristics. Rock geochemical analysis was carried out in the good soil geochemical anomalous area to further an?alyze its mineralization. Combined with field geological investigation, the authors preliminarily summarized the geochemical exploration model and prospecting orietation of the main ore?forming elements. Studies show that Jinhuasi surveyed area has Ag, Au geochemical a?nomalies, which are closely related to fault activity and diabase veins. The mineralization of the anomalous area is promising, with the surface mineralization of the first Ag mineralization anomalous surface being most excellent; nevertheless, the deep prospecting poten?tial remains uncertain.