中国铜矿床成矿期划分及其时空分布特征  

Metallogenic period division and time-spatial distribution of copper deposits in China

作　　者：王科强[1] 黄辉[1] 王治华[1] 喻万强[1] 张国利[1] 

机构地区：[1]武警黄金地质研究所,河北廊坊065000

出　　处：《矿产与地质》2006年第6期583-589,共7页Mineral Resources and Geology

摘　　要：根据全国1085个主要铜矿床的成矿时代研究,将中国铜矿床划分为前寒武纪、早古生代、晚古生代、三叠纪、侏罗-白垩纪、新生代六个成矿期。统计分析了各成矿期形成的铜矿床数量,在分析各成矿期地质演化历史的基础上,总结了不同矿床类型铜矿床的时间、空间分布特征。According to the study on the ore forming times of 1085 major copper deposits, the copper deposits in China have been divided into six metallogenic periods of Precambrian, Early Paleozoic, Late Paleozoic, Trias, Jurassic-Cretaceous and Cenozoic Era. The amount of copper deposits formed in different metallogenic eras was counted and analyzed. The time-spatial distribution characteristics of different types of copper deposit were summarized based on the analysis on the geological evolution history of different metallogenic periods.

关 键 词：铜矿床 时空分布特征 成矿期划分 古构造环境 矿床类型 中国 

分 类 号：P618.41[天文地球—矿床学]