王义文.金矿活化成矿论(以华北地台北缘为例)[J].地质找矿论丛,1992,(1):81-92
金矿活化成矿论(以华北地台北缘为例)
REMOBILIZATION METALLOGENY FOR GOLD DEPOSITS IN MARGIN OF THE NORTH CHINA PLATFORM
  
DOI:10.6053/j.issn.1001-1412.1992.1. 008
中文关键词:  华北地台  金矿化集中区  潜在含金性  继承性  构造动力成矿
英文关键词:
基金项目:国家“七五”重点科技攻关75-55-04-06专题所获主要理论成果之一
作者单位
王义文 中国有色金属工业总公司吉林矿产地质研究所 
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中文摘要:
      硫、铅同位素研究表明,金矿成矿作用具有明显的继承性.区域潜在含金性是形成金矿化集中区的首要前提,花岗岩类侵入体和韧性剪切带的形成是造成矿源层(岩)中金活化的主要营力.正常的岩浆结晶分异作用难以形成含金热液,通过二次活化再成矿是金矿成矿的主要机制.在成因上同时与太古宙绿岩建造和显生宙花岗岩类有关的一系列金矿床构成了地台区特有的金矿床系列.
英文摘要:
      Studise of sulphur & lead isotope have shown that there exists a remarkable inheritance in gold mineralization. The potential gold-bearing nature of certain region is the major premise of the formation of gold mineralization concentrate zones. The intrusion of granites & ductile shear zone are the main agents for the gold remobilization from source bed (rock). The common differentiation of magmatic crystallization is diffecult to generate auriferous hydrothermal solution. The basic mechanism of gold metallogeny is characterized by double remobilization & concentration of gold. A series of gold deposits related to both Archaen green stone formation & Phanerozoic granites constitute the characteristic gold deposit series in platforms.
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