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作 者:付洋[1] 王建新[1] 王超[1] 孙振明[1] 丁培超[2] 臧兴运[3]
机构地区:[1]吉林大学地球科学学院 [2]长春工程学院 [3]吉林省地质调查院
出 处:《黄金》2010年第4期18-22,共5页Gold
摘 要:古马岭金矿区是吉林省东南部重要的金成矿区之一,通过该区控矿地质条件的研究,结合水系沉积物测量、土壤地球化学测量、岩石地球化学测量及地球物理激电扫面开展靶区预测及找矿工作。研究表明:大东岔组片麻岩段应为金的矿源层,矿化带的宽度与金矿带的数量及品位成正比,断裂发育地段或不同方向断裂交汇部位是金的有利富集部位,晚侏罗世细粒闪长岩对矿区内金元素的富集提供热源和载体的作用,物化探异常与已知矿化蚀变带吻合较好。在此基础上,圈定A类预测区2处(其中包括高丽墓沟金矿床),B类预测区1处,C类预测区2处。The Gumaling gold deposit is one of the important gold deposits in southeast Jilin province.Based on the ore-controlling geological conditions research of the area,the target prediction and prospecting is carried out combining with the stream sediment survey,soil geochemical survey,lithogeochemical survey and geophysics IP scanning work.Studies show:the Dadongcha group gneiss paragraph is the gold ore source bed;and the mineralized belt width is proportional to the gold belt quantity and grade;faults and fault intersections in different directions is the gold enrichment sites;late Jurassic fine-grained diorite provides heat and carrier for the gold element enrichment.Geophysical and geochemical anomalies accord with the known mineralized alteration belts.2 A class prediction area(which includes the Gaolimugou gold deposit),1 B class and 2 C class prediction district are delineated.
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