摘要
本文以 1997年～ 1998年间 ,由中南工业大学与永平铜矿联合开展的矿区外围地质找矿项目的工作成果为基础 ,从成矿地质条件和矿化控制因素等方面 ,探讨了江西永平铜矿床是以晚古生代同生喷流沉积成矿作用为主体 ,并伴有其它成矿作用为特点的多因复成矿床。
Based on geological prostecting near the ore district in 1997~1998, Central&South University and Yongpin Copper Mine jointly launching, from mineralization geological condition and ore-controlling and etc., it is discussed that the deposit is an toly genetic compound one. The author indicated that syngenetic plume-sedimentation, in late-paleozoic era is primary in the deposit genesis, and other mineralization is secondly.
出处
《铜业工程》
CAS
2001年第3期48-50,共3页
Copper Engineering
关键词
矿床成因
喷流沉积成矿
铜矿床
Mineralization genesis Plume-sedimentation Yongpin copper deposit
