CAJ | 학술논문

桃园铜矿床位于内丘县与临城县交界处，大地构造位置属中朝准地台的山西断隆东部，太行山拱断束赞皇穹断束西侧。本文在“外宏观观测的基础上，对采集的岩矿石手标本及其对应的光、薄片进行了详细的分析鉴定，对其矿石矿物进行了系统的研究。根据矿物组合特征和矿物间的穿插关系，划分了成矿期次，进而认为该矿床的成矿过程可以分为热液成矿期和表生期。
도완동광상위우내구현여림성현교계처，대지구조위치속중조준지태적산서단륭동부，태행산공단속찬황궁단속서측。본문재“외굉관관측적기출상，대채집적암광석수표본급기대응적광、박편진행료상세적분석감정，대기광석광물진행료계통적연구。근거광물조합특정화광물간적천삽관계，화분료성광기차，진이인위해광상적성광과정가이분위열액성광기화표생기。
Taoyuan copper deposit is located in the junction of Neiqiu county and Lincheng County, tectonic position of it is Sino Korean Para platform Shanxi fault uplift, Taihang Mountain East, Zanhuang dome arch broken beam off beam on the west side. Its ore minerals were systematically studied on the basis of thin section and polished section microscope observation, According to the geological features, mineral characteristics and penetration relationship of minerals, the authors have made division of metallogenetic period and stages,and then consider the mineralization process can be divided into the deposit of hydrothermal mineralization and supergene period.