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
《地质找矿论丛》
CAS
CSCD
1999年第3期25-33,共9页
Contributions to Geology and Mineral Resources Research
基金
国家攀登计划项目
关键词
大型金矿
原生叠加晕
盲矿预测
金矿床
large size Au deposit
primary halo overprinting
ideal model
criteria for predicton of blind Au deposit
