摘要
论述了金矿多期多阶段叠加成矿成晕的地质地球化学特征。在研究大型金矿床原生叠加晕模型的基础上 ,建立了大型金矿床的原生叠加晕理想模型及盲矿预测准则。
The paper deals with geochemical characteristics of ore forming and halo forming processes of Au deposits with several metallogenic stages. Ideal model of primary halo overprinting and criteria for prediction of large size blind Au deposits are established on studies of modeling the primary halo overprinting of large size Au deposits.
出处
《黄金科学技术》
2001年第3期1-4,共4页
Gold Science and Technology
关键词
原生叠加晕
理想模型
盲矿预测准则
金矿床
large size Au deposit
primary halo overprinting
ideal model
criteria for prediction of blind Au deposit
