河北省张全庄金矿黄铁矿的标型特征及其成因意义  

The typomorphic characteristics andtheir genetic meaning on the pyrite of Zhang-Quan-Zhuang Gold Ore Deposit in Hebei Province

作　　者：银剑钊[1] 史红云[1] 

机构地区：[1]中国地质大学

出　　处：《黄金》1994年第1期6-11,共6页Gold

摘　　要：本文通过对张全庄金矿黄铁矿的形态及粒度标型、成分标型、晶胞参数标型、热电性标型的综合研究表明，张全庄金矿形成于中高温、中深成及硫逸度相对较高的地质环境。矿床为变质热液型金矿，但带有其它热液的叠加成因特征，即张全庄金矿应为多因复成矿床，这与张全庄金矿复杂的产出地质背景一致。On the basig of the study on the form,grade,composition, unit cellparameters and pyroelectricity of the pyrite of Zhang-Quan-Zhuang Oold Deposit,the authors of this paper conclude that Zhang-Quan-Zhuang Gold Deposit wasformed in the medium-high temperature and medium-deep environment. That isto say, this deposit is a metamorphic mesothermal gold ore deposit, however, ithas the characteristics of superimposed genesis of other kind hydrothermalism.It ought to be multi-genetic gold deposit.Thia is consistent to the complicatedbackground of the gold deposit.

关 键 词：金矿 黄铁矿 矿物标型 矿床成因 

分 类 号：P618.51[天文地球—矿床学]