CAJ | 학술논문

通过对卡邦加铜镍硫化物矿床近年来研究成果的初步总结，系统分析整理了矿床的地质特征，如矿体分布形态、矿石特征和矿体地球化学特征等。作者认为卡邦加铜镍硫化物矿床是超基性岩体侵入基巴拉带（卡拉圭-安科连）变质沉积岩内形成的贯入式岩浆融离型矿床。其矿体位于超基性岩底部，并与变质沉积岩一同经历后期的碰撞造山作用。矿体中的S主要来源于上地壳变质沉积岩。
통과대잡방가동얼류화물광상근년래연구성과적초보총결，계통분석정리료광상적지질특정，여광체분포형태、광석특정화광체지구화학특정등。작자인위잡방가동얼류화물광상시초기성암체침입기파랍대（잡랍규-안과련）변질침적암내형성적관입식암장융리형광상。기광체위우초기성암저부，병여변질침적암일동경력후기적팽당조산작용。광체중적S주요래원우상지각변질침적암。
The authors summarized previous research results of the Kabanga Ni-Cu sulphide deposits in north-western part of Tanzania. They analyze its geological characteristic, including the orebody shape, ore characteris-tics and geochemical characteristics,and suggest that the kabanga Ni-Cu sulphide deposit is a type of in-trused-Magmatic segregation deposit. The high MgO mafic-ultramafic magma intruded the metasedimentary rocks of the Kibaran Melt (Karagwe-Ankolean) along conduits and emplaced in the lowest of mafic-ultramafic in-trusions and then the deposits folded with the sedimentary rocks of the Kibaran Melt. The S of the kabanga Ni sul-phide deposits might be caused from the upper crustal material-the metasedimentary rocks of Karagwe-Ankolean.