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机构地区:[1]河北省区域地质矿产调查研究所,河北廊坊065000
出 处:《甘肃冶金》2016年第3期73-77,共5页Gansu Metallurgy
摘 要:满都胡宝力格地区位于朝不愣-查干敖包铁锌铅成矿带内,已发现查干敖包锌铁多金属矿床、巴润必鲁特铅锌银多金属矿点10余处,成因类型以火山热液型为主。在对区域地质背景、矿床时空展布规律研究基础上,探讨了地层、构造、岩浆岩与成矿的关系。根据研究区内各类矿产的成矿地质背景、时空分布规律、控矿条件以及化探异常分布特点等因素,将区内划分为4个成矿亚带,圈出9个成矿远景区,12个找矿靶区。Manduhubaolige area is located in the zinc-iron metallogenic belt of Chaobulen-Chaganaobao. More than 10 de- posits, such as Chaganaobao zinc-silver polymetallic deposits and Baryunbilute Lead-zinc-silver deposit, have been found. The occurrence is primarily volcanic hydrothermal type. Discussion is made on the formation, structure, magmatic rocks and mineralization. Based on metallogenic geological settings and the time-space distribution rule, the ore-controlling condi- tions, and the distribution characteristics and geochemical anomalies, the area it is divided into four sub metallogenic belts, 9 metallogenic prospecting zones and 12 prospecting target zones in this area were delineated.
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