摘要
Abstract
Qiaozikeng lead-zinc deposit located in the central eastern part of the Yinkeng precious metal ore field in Yudu County,Jiangxi Province,The geological structure of Qiaozikeng lead-zinc deposit is located in the southern section of the Yanshanian tectonic basin from Yudu Yinkeng to Ningdu Qingtang in the eastern part of southern Jiangxi,it also located at the junction of the Wuyi block and the Luoxiao block.Through shallow surface engineering and a small amount of deep drilling engineering,Five fractured altered rock type gold-silver-lead-zinc mineralization zones and two stratabound gold-silver-lead-zinc mineralization belts have been identified.The Qiaozikeng lead-zinc deposit occurs in the Shangshi group of the Nanhua formation and the Kuri group of the Qingbaikou formation.It is controlled by multiple factors such as stratigraphy,fault structures,and fold structures,and the deposit types are divided into two types:fractured altered rock type and layer controlled type.Finally,it was determined that the deep part of the mining area has significant mineralization potential and can be used as the next direction for mineral exploration.关键词
铅锌矿床/地质特征/找矿方向/桥子坑/江西省Key words
lead-zinc deposit/geological characteristics/prospecting direction/Qiaozikeng/Jiangxi Province分类
天文与地球科学
