摘要
据钟丘洋火山热液型铜矿床的地层、侵入岩、矿石和矿体中元素的分布规律，阐明了该矿床的地球化学原生异常特征；确定了与矿床有关的指示元素及其分带序列；建立了矿床剥蚀程度的评价指标及该矿床的地球化学异常模式。
According to distribution regularity of elementS in strata, intrusive rocks, ores and orebodies of theZhongqiuyang volcanogene hydrothermal copper deposit, this paper has elucidated characteristics of geochemical primary anomalies, determined indicator elements related to the ore deposit and their sequence of zoning, established indices for evaluating denudation extent of ore deposit, and formulated geochemical anomaly pattern of the ore deposit.
出处
《物探与化探》
CAS
CSCD
1997年第5期331-338,共8页
Geophysical and Geochemical Exploration
关键词
铜矿床
热液型
火山
地球化学
hydrothermal copper deposit, anomaly characteristics, anomaly pattern
