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吉林通化南岔式金矿地质—地球物理—地球化学综合找矿模型 被引量:15

Integrated geological-geophysical-geochemical ore prospecting model of the Nancha-style gold deposit in Tonghua,Jilin
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摘要 老岭成矿带为吉林省最重要的贵金属、有色金属成矿带,南岔金矿是该成矿带近几年新发现的金矿床。在阐述南岔金矿成矿地质条件、岩(矿)石物性参数特征、地球物理场、地球化学特征的基础上,归纳并提取了控矿地质因素和物化探找矿标志,从而建立了“南岔式”金矿的地质—地球物理—地球化学找矿模型。 The Laoling metallogenic belt is the most important noble metal and nonferrous metal metallogenic belt in Jilin Province and the Nancha gold deposit is a gold deposit found in recent years in this metallogenic belt.On the basis of studies of the metallogenic-geological conditions ,rock(ore)physical parameters,geophysical field and geochemical characteristics of the Nancha gold deposit,the author has summarized and extracted the ore-control ling fac-tors and geophysical and geochemical ore guides and constructed a geological-geo physical-geo-chemical ore-prospecting model of Nancha-style gold deposits.
作者 关键
出处 《中国地质》 CAS CSCD 2001年第12期22-29,42,共9页 Geology in China
关键词 南岔金矿床 找矿模型 “S”型断裂 地球物理 地球化学 Nancha gold deposit ore-prospecting model S-shaped fault geophysics geo-chemistry
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  • 1B. N. Eisenlohr,D. Groves,G. A. Partington. Crustal-scale shear zones and their significance to Archaean gold mineralization in Western Australia[J] 1989,Mineralium Deposita(1):1~8
  • 2S. Berglund,T. K. Ekstr?m. Arsenopyrite and sphalerite as T-P indicators in sulfide ores from northern Sweden[J] 1980,Mineralium Deposita(2):175~187

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