CAJ | 학술논문

上金山钨钼矿位于安徽省绩溪县与旌德县交界地带，是扬子准地台南缘新发现的一处大型层控型矿床。南华系休宁组上段上部地层及燕山早期的花岗闪长岩是本矿床主要控矿因素，赋矿地层岩性为锰钙质砂岩-粉砂岩，该赋矿层位是皖南地区找矿新发现。该矿床已达大型规模，地质、物化探综合信息显示，上金山地区具进一步找矿前景，且在已控制的层控型矿床深部及外围，存在寻找斑岩型钨钼矿及石英脉型钨矿的良好条件，经进一步勘查，矿床资源量将显著增加。
상금산오목광위우안휘성적계현여정덕현교계지대，시양자준지태남연신발현적일처대형층공형광상。남화계휴저조상단상부지층급연산조기적화강섬장암시본광상주요공광인소，부광지층암성위맹개질사암-분사암，해부광층위시환남지구조광신발현。해광상이체대형규모，지질、물화탐종합신식현시，상금산지구구진일보조광전경，차재이공제적층공형광상심부급외위，존재심조반암형오목광급석영맥형오광적량호조건，경진일보감사，광상자원량장현저증가。
The Shangjinshan Wo-Mo ore deposit lies in beween Jixi County and Jinde County of Anhui Province, is a large strata-bound ore deposit found at the southern fringe of the Yangtze paraplatform. The upper part of the upper member of Xiuning Formation of Nanhua System and the early Yanshanian granodiorite are major ore-control factor of this deposit, and the lithology of ore host is Mn-Ca sandstone-siltstone, which is a new discovery as an ore host in south Anhui. The deposit is big in size. Geological, geophysical and geochemical information as a whole indicates that there is more potential in the Shangjinshan area, and in the depth and periphery of the already controlled strata-bound deposit, there exist good conditions for exploration of porphyry W-Mo ore and quartz vein W ore deposit, after further exploration, the resources will be increased remarkably.