CAJ | 학술논문

哈萨克斯坦北天山金矿床成矿作用时间为二叠纪末至三叠纪，是天山晚期后碰撞阶段的产物，具典型的低硫型浅成低温热液金矿床特征。区内矿床受构造-火山岩共同控制，矿床以火山穹隆为中心沿NE向破碎带形成规模较大的矿体，沿NW向和近EW向形成小矿体，在交叉部位形成厚大的富矿体。在垂向上地表以金银矿化为主，向深部过渡为铜铅锌矿化，底部演变为含铜矿化侵入岩脉。
합살극사탄북천산금광상성광작용시간위이첩기말지삼첩기，시천산만기후팽당계단적산물，구전형적저류형천성저온열액금광상특정。구내광상수구조-화산암공동공제，광상이화산궁륭위중심연NE향파쇄대형성규모교대적광체，연NW향화근EW향형성소광체，재교차부위형성후대적부광체。재수향상지표이금은광화위주，향심부과도위동연자광화，저부연변위함동광화침입암맥。
Metallogenic age of Kazakhstan North Tianshan gold deposit is from lower Permian to Triassic,it is results of the late Tianshan collision stage,with typical character of low sulfur type epithermal gold deposits. The deposit is con-trolled by tectonic - volcano rock, The volcano dome as the center of desposit with Northeast fracture zone formed large ore bodies,norhwest and sublatitudinal formed small orebody in trend,and formed thick rich orebody in cross section; In the vertical direction, shallow to gold-silver mineralization, into the deep transition for the copper -lead- zinc mineraliza-tion, the bottom for the evolution of intrusive rock stock with containing copper mineralization.