CAJ | 학술논문

唐家湾钒钛磁铁矿位于扬子陆块与松潘—甘孜活动带的西南结合部康滇断隆带中段南部、安宁河断裂西侧。矿体产于华力西期基性超基性岩体中，矿石矿物主要为钛磁铁矿、钛铁矿等，多具海绵陨铁结构，在岩浆结晶晚期形成，围岩为印支期正长岩。矿床成因为晚期岩浆矿床。
당가만범태자철광위우양자륙괴여송반—감자활동대적서남결합부강전단륭대중단남부、안저하단렬서측。광체산우화력서기기성초기성암체중，광석광물주요위태자철광、태철광등，다구해면운철결구，재암장결정만기형성，위암위인지기정장암。광상성인위만기암장광상。
The Tangjiawan Vanadio-titano-magnetite deposit lies in the south of middle section of the Kangdian fault upwarping belt and on the western side of the Anninghe Fracture zone. The orebodies are confined to Hercynian ultrabasic rock. The ore consists of titanomagnetite and ilmenite with sideronitic texture. The deposit belongs to late magmatic ore deposit.