金厂峪金矿床围岩蚀变特征与矿床成因  

CHARACTERISTICS OF ALTERATION AND GENESIS OF THE JINCHANGYU GOLD DEPOSIT

作　　者：秦大军[1] 蔡新平[1] 王杰[1] 周以柏 祁学义 郝荣 

机构地区：[1]中国科学院地质研究所

出　　处：《贵金属地质》1999年第1期7-14,共8页

摘　　要：为了更深入地理解金厂峪金矿床成矿作用，对该金矿床内蚀变围岩的矿物组合、成分及其变化进行了较详细的研究．蚀变带质量平衡分析表明Ａｌ２Ｏ３、ＭｎＯ、Ｐ２Ｏ５等组分具不活动性．由蚀变围岩向钠长石英脉，在蚀变岩中元素无明显变化．钠长石英脉体的形成与围岩蚀变有关，但两者成因并不相同．Characteristics of the alteration and zonation of gold deposits play an important role in acquiring the composition and feature of ore forming fluid,the contribution of wall rocks and the origin of gold deposits.According to the mineral association,composition and their variations in Jinchangyu gold deposit,four alteration zones can be recognized away from gold bearing quartz zones,i.e.,weakly altered zone,chloritized zone,sericitized zone and silicifized zone.The mass balance analysis for the altered rocks of the Jinchangyu gold deposit shows that Al 2O 3 has obvious immobility.The chemical composition of the altered rocks is normalized with the content of Al 2O 3 in the weakest altered rock,and the standardized corresponding composition differences between the weakest altered rock and other altered rocks indicate the composition variations during the interaction between wall rocks and the ore forming fluids.The calculating results suggest that the contents of SiO 2,FeO,CaO,MgO,Sr,Ba,Sc,Zn,Ga,Ta,Au,Ag,Y and Pb in gold bearing quartz veins are much higher than those in the altered rocks,and SiO 2,Sr and Ba in the altered rocks have an obvious increase relatively to their original rocks in contrary to FeO,CaO,MgO,Sc,V,Y,Pb,P and Cu.The composition of the altered rocks from the weakly altered rocks to gold bearing quartz veins in the Jinchangyu gold deposit varies irregularly.The composition variation in the altered rocks is not related to the increase of the corresponding composition in the gold bearing vein,and it has minor effects on the composition of ore forming fluid.Despite the existence of some genetic relation,the gold bearing quartz veins and altered wall rocks would form in different conditions.During alteration,wall rocks might release too limited ore forming elements in quantity to form a large scale gold deposit.Hence,the ore forming material of the Jinchangyu gold deposit should be mainly derived from deep source ore forming fluid.

关 键 词：蚀变岩 含矿脉带 金矿床 矿床成因 

分 类 号：P618.510.1[天文地球—矿床学] P618.510.2[天文地球—地质学]