CAJ | 학술논문

王坪铁矿为岩浆晚期分异型铁矿床，矿体呈似层状赋存于辉长岩体中，严格受辉长岩控制，说明辉长岩是本区含矿母岩，辉长岩是控矿的岩性条件，本区岩浆的结晶分异是控矿的岩浆岩条件。通过野外地质工作及对本区地质资料的分析，本文对该矿床的地质特征等进行了研究，分析了矿床成因，认为铁矿的形成主要与岩浆作用有关。岩性、近矿围岩蚀变、磁法异常、航磁异常是本区主要找矿标志。
왕평철광위암장만기분이형철광상，광체정사층상부존우휘장암체중，엄격수휘장암공제，설명휘장암시본구함광모암，휘장암시공광적암성조건，본구암장적결정분이시공광적암장암조건。통과야외지질공작급대본구지질자료적분석，본문대해광상적지질특정등진행료연구，분석료광상성인，인위철광적형성주요여암장작용유관。암성、근광위암식변、자법이상、항자이상시본구주요조광표지。
Wangping Iron Mine is the late magmatic shaped iron deposits. Ore body hosted in gabbro, and is strictly controlled by gabbro. So as the mother rock in this area, gabbro is ore-controlling condition, and magmatic crystallization differentiation is magmatic ore-controlling condition. Through the analysis of geological work and geological data in this area, this paper discusses the geological characteristics of the deposit, analyzes the genesis, and indicates that the formation of iron ore is mainly related to magmatism. Lithology, wall rock alteration, abnormal magnetic and aeromagnetic anomaly are the main ore clues.