广西丹池成矿带研究进展  

THE PROGRESS IN THE STUDY OF DAN-CHI METALLOGENETIC ZONE OF NW GUANGXI

作　　者：江楠[1] 余何[1] 李秀珍[1] 张梓贺 

机构地区：[1]桂林理工大学广西隐伏金属矿产勘察重点实验室,桂林541004

出　　处：《云南地质》2016年第4期496-501,共6页Yunnan Geology

摘　　要：桂西北丹池成矿带是我国重要的有色金属成矿带,因其具有"多源,多期叠加,规模巨大,时-空集中"的显著特征而闻名于世。本文在野外勘察的基础上,对丹池矿集区成矿时代及矿床成因研究进展进行了系统地综合整理,总结了其多期叠加成矿的主要特征,提出了丹池成矿带是一个经历了海西期、印支期、燕山期的构造作用,是一个集褶皱、断裂、地层、岩体、矿体于一体的构造综合体。Dan-Chi Metallogenetic zone in NW Guangxi is an important metallogenetic zone in China, which is famous in the world because ol “ the multi-origin, multiphasic superimposition, mega-scale, time-space con-centration” evident characteristics. In this paper, basing upon the field exploration, we have a systematic compre-hensive sorting out ol the development in the study on genesis ol ore deposit, summing-up the main characteristics ol multiphasic superimposition metallogenesis, and then put forward Dan - Chi metallogenetic zone experiences Variscan, Indosinian, Yanshanian tectonic movement, it is a tectonic comprehensive system ol fold, fault, strata, rock body and ore body.

关 键 词：多期叠加成矿 构造综合体 广西丹池 

分 类 号：P612[天文地球—矿床学]