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新疆阿吾拉勒陆相火山岩型铜矿成矿研究
引用本文:莫江平,黄明扬.新疆阿吾拉勒陆相火山岩型铜矿成矿研究[J].矿产与地质,1996,10(4):217-223.
作者姓名:莫江平  黄明扬
作者单位:中国有色金属工业总公司矿产地质研究院
基金项目:“八五”国家三○五项目
摘    要:阿吾拉勒陆相火山岩型铜矿分为火山热液型、次火山热液型和中低温热液充填脉型,认为岩浆和成矿物质来源于深部地壳或上地幔,成矿与华力西晚期火山一次火山作用密切相关,铜矿是在同一构造环境下同一岩浆源分异演化不同阶段的产物。矿床成因属中低温火山一次火山热液成因。

关 键 词:火山岩  铜矿床  成因  成矿

GENESIS OF CONTINENTAL VOLCANIC TYPE COPPER DEPOSITS IN AWULALE,XINJIANG
Mo Jiangping,Huang Mingyang,Qin Longfang and Lu Hanti.GENESIS OF CONTINENTAL VOLCANIC TYPE COPPER DEPOSITS IN AWULALE,XINJIANG[J].Mineral Resources and Geology,1996,10(4):217-223.
Authors:Mo Jiangping  Huang Mingyang  Qin Longfang and Lu Hanti
Abstract:The Awulale copper deposit can be classified into volcanic hydrothermal type,subvolcanic hydrothermal type and middle lower temperature hydrothermal filling vein type,It is considered that the magma and mineralization materials were from deep crust or upper mantle,that the mineralization was closely related to the late Variscan volcanic subvolcanism,and that the copper was resulted in the different stages of differentiation and evelotion of the same magma source in the same tectonic setting.The genetic type belongs to volcanic subvolcanic hydrothermal type with middle low temperature.
Keywords:Continental volcanic rock  Copper deposit  Genesis  Xinjiang  
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