白银厂铜多金属矿田地球化学研究进展  

Progress of geochemical research in Baiyinchang Cu-polymetallic ore field

作　　者：郭凯凤 陈守余[1,2] GUO Kaifeng;CHEN Shouyu(Faculty of Earth resources,China University of Geosciences,Wuhan 430074,China;State Key Laboratory of Geology Processes and Mineral Resources,China University of Geosciences,Wuhan 480074,China)

机构地区：[1]中国地质大学(武汉)资源学院,武汉430074 [2]中国地质大学地质过程与矿产资源国家重点实验室,武汉430074

出　　处：《地质找矿论丛》2018年第4期517-526,共10页Contributions to Geology and Mineral Resources Research

基　　金：中国地质调查局科研项目"甘肃省白银厂影响找矿突破的关键地质问题及找矿预测研究"(编号:12120114050101)资助

摘　　要：白银厂铜多金属矿田是上世纪五十年代初期在我国西部发现并勘探成功的大型铜矿区。随着现代测试分析技术的进步,矿床地球化学研究取得明显进展。本文主要论述了其中的几个方面,包括微量元素地球化学、矿床同位素地球化学、成矿年代学等方面的某些研究进展。The Baiyinchang Cu -polymetallic ore field is a large copper ore area discovered in the West China. It has been successfully explored in the early 50s of last century. With development of modern test and analysis technology, remarkable progress has been made in the study of the geochemistry of ore deposits there. This paper discusses mainly research progress of the aspects including trace element geochemistry, isotope geochemistry of ore deposits, metallogenic geochronology etc.

关 键 词：铜多金属矿床 微量元素地球化学 矿床同位素地球化学 成矿年代学 白银厂 甘肃省 

分 类 号：P618[天文地球—矿床学]