摘要
简要分析了青城子金、银、多金属矿田成矿地质背景,重点阐述了控矿因素,认为原始断陷盆地控制并聚积了丰富的成矿物质,后期地质事件对成矿物质的活化与聚积有直接影响,矿床类型及其空间分带与沉积环境相关。概括出矿田地质找矿标志,明确指出该区找矿方向。
The article briefly analyses the ore forming geological background, focusing on the ore controlling factor. .The author thinks the original fault depression basin controls and concentrate s abundant ore forming materials. The later geological changes influenced the activation and concentration .The deposit types and their distribution are related with the deposit environment .It also points out the ore finding sign and ore finding direction.
出处
《矿产与地质》
2005年第1期39-42,共4页
Mineral Resources and Geology
