摘要
在阐明成矿地质背景基础上，论述了崇安─宁化地区金锡多金属矿床成矿地质特征，并从成矿控制、矿床时空分布格局、成矿区域、成矿系列等方面总结了成矿规律。将崇安─宁化构造成矿带划分成3个成矿区，同时将全锡多金属矿床划分成三大成矿系列和6个矿床式。
Based on clarifying metallogenic geological background，metallogenic geological characters of gold－tin －polymetal deposits in Chong an－Ninhua area are expounded，and metallosenic rules are summarized on aspects of ore－controlling, temporary and spatial distribution patterns of mineral resources， ore－forming regions, ore－furming series． The Chongan－Ninhua structural metallogenic zone is divided into 3 ore－forming provinces， while the gold－tin－polymetal deposits are divided into 3 ore-forming series and 6 deposit types.
出处
《火山地质与矿产》
1995年第3期7-19,共13页
Volcanology & Mineral Resources
基金
地矿部"八.五"地质找矿科技攻关项目!85-01-004-9
关键词
成矿地质
成矿规律
金矿床
锡矿床
多金属矿床
metallogenic geological background, metallogenic geological characters, metallogenic rules，Chong'an-Ninhua
