CAJ | 학술논문

黔北冯家湾锰矿床严格受控于地层层位和古构造，本文总结分析了冯家湾锰矿矿床地质特征、矿石质量特征等方面进行了阐述，认为该矿床属浅海海湾相沉积型锰碳酸锰矿床，并提出该区找矿前景好，深部找矿潜力大，应该加大找矿力度。
검북풍가만맹광상엄격수공우지층층위화고구조，본문총결분석료풍가만맹광광상지질특정、광석질량특정등방면진행료천술，인위해광상속천해해만상침적형맹탄산맹광상，병제출해구조광전경호，심부조광잠력대，응해가대조광력도。
Fongjiawan manganese deposit is strictly controlled by strata and paleostructure and occurred as stratiform and quasi-stratiform. We firstly described the geologic character of the deposit and component of ores. Then according to the study on sedimentary environment of the manganese deposit, we concluded that the deposit belong to sediment carbonate type manganese deposit which formed in shallow-sea facies. As a result, it has a huge potential on prospecting perspective.