摘要
Abstract
Anlin iron mine are mainly skarn ( contact metasomatic) iron ore, which is produced in the contact zone of acidic - intermediate mafic intrusive rocks and calcium magnesian carbonate rocks. It has large area, stable layer and good ore forming conditions. So it has good prospecting potential. The author attempts to look for iron ore enrichment regularity from its geological characteristics and metallogenic regularity to provide theoretical basis for future prospecting and exploration.关键词
接触交代型铁矿/地质特征/成矿规律/李珍铁矿Key words
contact metasomatic iron deposit/ geological characteristics/ metallogenic regularity/ Lizhen Iron Deposit分类
天文与地球科学
