(中國有色金屬工業(yè)總公司北京礦產(chǎn)地質(zhì)研究所，北京 100012)
摘 要: 系統(tǒng)地論述了華北地臺南緣不同類型金礦床的硫、 鉛、 氫、氧和碳同位素地球化學(xué)，指出它們一致表明石英脈型和蝕變斷層巖型金礦床的成礦元素和介質(zhì)主要來自太古代變質(zhì)巖系，爆破角礫巖型金礦床的成礦元素和介質(zhì)則來燕山期鈣堿系列巖漿， 它們分別屬變質(zhì)熱液型和巖漿熱液型礦床。
關(guān)鍵字: 同位素地球化學(xué) 金礦床 成因 華北地臺南緣
（Beijing Institute of Geology for Mineral Resources, CNNC, Beijing 100012, P. R. China）
Abstract:The isotopic features of sulfur, lead, hydrogen, oxygen and carbon for different types of gold deposits in the southern margin of North China Platform were described in detail, which all unanimously indicated that the ore-forming elements and media of the gold deposits of quartz vein-type and altered rock-type derived from the Archean metamorphic series and their geneses belong to metamorphic hydrothermal type, and that of the deposits of explosive breccia type derived from the calc-alkaline magma and its genesis belongs to magmatic hydrothermal type. In the two types of derived deposits, the meteoric water participated in their formation.
Key words: isotopic geochemistry gold deposit genesis North China Platform
