(1.中南工業(yè)大學(xué)資源環(huán)境與建筑工程學(xué)院，長(zhǎng)沙 410083;
2.中國(guó)有色金屬工業(yè)總公司地質(zhì)總局，北京 100814)
摘 要: 論述了老廠(chǎng)礦床的大地構(gòu)造環(huán)境、 礦床地質(zhì)地球化學(xué)特征、噴流巖特征和成礦溫度，劃分了礦化期和礦化階段，認(rèn)為老廠(chǎng)礦床應(yīng)屬瀾滄裂谷(斷拉谷)中海底火山噴流沉積型并迭加隱伏巖漿熱液改造型礦床，建立了“三層樓” 成礦模式。對(duì)今后找礦勘探工作具重要的理論指導(dǎo)意義。
關(guān)鍵字: 塊狀硫化物礦床 礦床成因 成礦模式
（1.College of Resource, Environment and Civil Engineering, Central South University of Technology, Changsha 410083;
2.The General Geologic Prospecting Bureau, CNNC, Beijing 100814）
Abstract:The geotectonic setting, the geology of ore deposits, geochemical and sedex rock characters and metallogenetic temperature were studied, as well as metallization phase and stages of mineralization of Laochang ore deposits. It was considered that the Laochang ore deposits should be contained in the submarine volcanic sedex-reformed deposits in Lancang rift. The "three-storey building pattern" metallogenetic model was established, which has important theoretical and guiding significances for the prospecting in future.
Key words: massive sulfide deposits genesis of deposit metallogenetic model
