期刊文献+

金厂峪金矿床围岩蚀变特征与矿床成因 被引量:4

CHARACTERISTICS OF ALTERATION AND GENESIS OF THE JINCHANGYU GOLD DEPOSIT
下载PDF
导出
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.
出处 《贵金属地质》 1999年第1期7-14,共8页
关键词 蚀变岩 含矿脉带 金矿床 矿床成因 altered rocks ore bearing veins\ metallogeny of Jinchangyu gold deposit
  • 相关文献

参考文献2

二级参考文献9

  • 1蔡新平,刘秉光,季钟霖,祁学义.金厂峪金矿的控矿构造及其地球物理验证[J].黄金科学技术,1994,2(5):1-7. 被引量:24
  • 2曲以秀,刘志国.冀东燕山期花岗岩成因及其与金矿化的关系[J].长春地质学院学报,1995,25(4):393-398. 被引量:9
  • 3刘瑾璇,河北省金厂峪金矿床地质条件研究及成矿靶区预测科研报告,1994年
  • 4涂光炽,地学前缘,1994年,1卷,3期,45页
  • 5宋瑞先,河北金矿地质,1994年
  • 6许云程,河北金厂峪金矿床成矿地质条件及深部矿体预测研究报告,1990年
  • 7杨国清,构造地球化学,1990年
  • 8张秋生,冀东金厂峪地区高级变质区地质与金矿床,1990年
  • 9余昌涛,中国金矿床主要类型区域成矿条件文集.2,1989年

共引文献15

同被引文献41

引证文献4

二级引证文献13

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部