CAJ | 학술논문

焦家金矿属于蚀变岩型金矿，围岩蚀变发育，是我国储量最大的金矿床之一。该文对蚀变带中的钾长石的赋存状态、化学成分进行了分析研究，并与未蚀变的玲珑岩体中的钾长石进行对比。认为焦家金矿床主要存在三种成因类型的钾长石，即原生钾长石（岩浆成因）、高温热液钾长石、低温热液钾长石。结合前人的研究成果，探讨了热液钾长石的形成与成矿意义。
초가금광속우식변암형금광，위암식변발육，시아국저량최대적금광상지일。해문대식변대중적갑장석적부존상태、화학성분진행료분석연구，병여미식변적령롱암체중적갑장석진행대비。인위초가금광상주요존재삼충성인류형적갑장석，즉원생갑장석（암장성인）、고온열액갑장석、저온열액갑장석。결합전인적연구성과，탐토료열액갑장석적형성여성광의의。
Jiaojia gold deposit belongs to altered rock type gold deposit,which has extensive wall rock al-teration.It is one of the biggest gold deposit in reserves.Occurrence and chemical composition of the K feldspar in the alteration rock have been analyzed and studied,and compared with the K feldspar in the non alterated Linglong rock bodies.Three genetic types of K feldspar occurred in Jiaojia gold deposit, including native K feldspar (magmatic origin),hydrothermal K feldspar of high temperature and hydro-thermal K feldspar of low temperature.Finally,combining with previous research,the formation and its mineralization significance of the hydrothermal K feldspar have been discussed.