CAJ | 학술논문

帕奔金矿床赋存于古生界二叠系灰岩中及与之相邻的接触带上。矿床受NNW向脆性断裂的控制，区域内构造发育，成矿条件优越。在前人研究的基础上，以帕奔金矿床为研究对象，通过对矿区地质概况、金矿矿床的类型及特征等的研究，按照矿床矿体热液作用类型、矿体就位方式和地质环境可分为四类：构造蚀变岩型金矿、断层破碎角砾岩型金矿、热液充填碳酸盐脉型金矿、红土型或溶洞型金矿。总结出该区是以构造作用和围岩蚀变为主的控矿因素，且运用元素地球化学参数特征，以及地球化学异常组合的方法，获取了区域找矿标志，对以后该地区寻找金矿具有重要的指导意义。
파분금광상부존우고생계이첩계회암중급여지상린적접촉대상。광상수NNW향취성단렬적공제，구역내구조발육，성광조건우월。재전인연구적기출상，이파분금광상위연구대상，통과대광구지질개황、금광광상적류형급특정등적연구，안조광상광체열액작용류형、광체취위방식화지질배경가분위사류：구조식변암형금광、단층파쇄각력암형금광、열액충전탄산염맥형금광、홍토형혹용동형금광。총결출해구시이구조작용화위암식변위주적공광인소，차운용원소지구화학삼수특정，이급지구화학이상조합적방법，획취료구역조광표지，대이후해지구심조금광구유중요적지도의의。
Phabon gold deposit hosted in Permian Paleozoic limestones and the adjacent contact zone. Controled by NNW brittle fracture,the deposit structure developed in the region,and the metallogenic condition was superior. On the basis of the previous studies on Phabon gold deposit,the mining geology,gold deposit type and characteristics of the deposit were analyzed. According to the type of hydrothermal ore deposit,ore body in place ways and geological environment,it can be divided into four categories,structural alteration type gold deposits,broken fault breccia type gold deposits,hydrothermal filling carbonate vein type gold deposits,and laterite?type/cave?type gold deposits. We summed up that the tectonization and wall rock alteration are the main ore?controlling factors of the area. Based on the element geochemistry parameters characteristic,we used geochemical anomalies combined method to get the regional ore indications,providing important guidance for exploration gold deposits of the area in future.