云南广南县者龙锑矿地质特征及成因  

THE GEOLOGICAL FEATURE AND GENESIS OF ZHELONG SB DEPOSIT IN GUANGNAN,YUNNAN

作　　者：田犁平 罗云平 

机构地区：[1]云南省有色地质局三〇六地质队,云南昆明650217

出　　处：《云南地质》2015年第2期243-246,共4页Yunnan Geology

摘　　要：者龙锑矿受构造、地层岩性控制,成矿物质主要来源于版纳组。矿体主要赋存于断裂构造破碎带内,含矿岩性为构造角砾岩,蚀变标志明显,矿床成因属于断裂破碎带控制的低温热液矿床。Zhelong Sb deposit is controlled mainly by structure, bed character. The metallogenetic material is derived mainly from Banna Formation. The main ore body is in the fault fracture zone. The ore-bearing bed is structure breccias, with clear alteration criteria. It belongs to the low T hydrothermal deposit controlled by fault fracture zone in genesis.

关 键 词：断裂控矿 岩性控矿 低温热液矿床 

分 类 号：P618.66[天文地球—矿床学]