CAJ | 학술논문

矽卡岩型铁矿床在我国分布广泛，主要集中在河北省邯（郸）-邢（台）地区、鄂东、晋南、豫西、鲁中、苏北、闽南、粤北以及川西南、滇西等地，是我国富铁矿石的主要来源，矿床规模以中小型为主，个别为大型，是我国主要铁矿床类型之一。通过对上梁湾铁矿床矿体的地质特征、矿床成因及赋存规律等的研究，为豫西此类矿床的找矿和探矿提供资料，同时还能为矿山深部找矿勘查和工程布置提供参考。
석잡암형철광상재아국분포엄범，주요집중재하북성함（단）-형（태）지구、악동、진남、예서、로중、소북、민남、월북이급천서남、전서등지，시아국부철광석적주요래원，광상규모이중소형위주，개별위대형，시아국주요철광상류형지일。통과대상량만철광상광체적지질특정、광상성인급부존규률등적연구，위예서차류광상적조광화탐광제공자료，동시환능위광산심부조광감사화공정포치제공삼고。
Skarn type iron ore deposits are widely distributed in China,mainly distribute in Hebei Handan-Xingtai area,Eastern Hubei,Southern Shanxi,Western Henan,Central Shandong,Northern Suzhou,Southern Fujian,Northern Guangdong,Southwestern Sichuan and Western Yunnan. They are the main source of rich iron ore in China. As one of the main iron ore deposit types in China,they are mainly small and medium scale,and some large scale. Based on the research of geological characteristics,mineral deposit genesis,and distribution regular of Shangliangwan iron ore deposit,this study provides research data for prospecting and exploration of this type of ore deposits,and provides reference for prospecting and engineering of deep ore mining.