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作 者:马财 李华 崔召玉 汪鹏 于小亮 MA Cai;LI Hua;CUI Zhaoyu;WANG Peng;YU Xiaoliang(Qinghai Geological Bureau,Xining 810015,Qinghai,China;The Third Exploration Institute of Qinghai Nonferrous Geological Exploration Bureau,Xining 810012,Qinghai,China)
机构地区:[1]青海省地质调查局,西宁810015 [2]青海省有色地质勘查局第三勘查院,西宁810012
出 处:《地质找矿论丛》2024年第2期149-159,共11页Contributions to Geology and Mineral Resources Research
摘 要:裕龙沟铜镍矿床(小型)位于南祁连成矿亚带东段满隆山一带。成矿与区内基性-超基性岩体密切相关,属含铂族富铜镍矿床。本文基于对该区以往地质、磁法、电法及地气测量成果资料进行了较系统地分析研究,探索了成因机制,构建了相应成矿模式及找矿模型,并进行了成矿预测。结果表明,在裕龙沟矿区东侧的隆哇塞日登地区具有良好的成矿远景及找矿潜力;南祁连成矿带东段具备加里东晚期后碰撞伸展环境下的岩浆型铜镍硫化物矿床形成条件。The small sized Yulonggou Cu-Ni deposit located at Manlongshan area in the east section of the South Qilianshan sub-ore belt is closely related to basic-ultrabasic rock distributed in the area.And it is a PGE-bearing Cu-Ni deposit.Based on systematic analysis of data obtained from geological,magnetic,electric and geo-gas survey is discussed genesis of the deposit and built the metallogenic and prospecting models and made prospecting prediction.Longwa Sairideng area on the east side of Yulonggou area is prospective and potential for further prospecting.Metallogenic conditions of magmatic Cu-Ni sulfide deposit under Late Caledonian post collision extensional environment exist in the eastern part of South Qilianshan ore belt.
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