江西垄里甘锡多金属矿地质特征及矿床成因分析  

Geological characteristics and genetic analyses of Tin-polymetallic ore deposit in Longligan,Jiangxi Province

作　　者：张园 万梦 欧阳学财 杨立飞 ZHANG Yuan;WAN Meng;OUYANG Xuecai;YANG Lifei(The Third Geological Brigade of Jiangxi Geological Bureau,Jiujiang 332100,Jiangxi,China;Jiangxi Natural Resources Policy Survey and Evaluation Center,Nanchang 330000,Jiangxi,China;East China University of Technology,Nanchang 330013,Jiangxi,China)

机构地区：[1]江西省地质局第三地质大队,江西九江332100 [2]江西省自然资源政策调查评估中心,江西南昌330000 [3]东华理工大学,江西南昌330013

出　　处：《矿产勘查》2024年第S2期425-431,共7页Mineral Exploration

基　　金：江西省国土资源厅地质勘查基金项目“江西省德安县垄里甘锡多金属矿预查”(20160010)资助。

摘　　要：垄里甘锡矿区处于扬子准地台内九江台陷—九江褶断束南缘,其南部与江南台隆相邻,位于彭山穹隆构造的东侧,是长江中下游彭山锡矿田内重要的锡矿床之一。本文在前人区域研究的基础上,通过对垄里甘锡矿床的地质特征、控矿因素和找矿标志进行分析总结,从而探讨锡矿床成因,以便进一步指导彭山地区此类型锡矿的找矿工作,也为该矿区下一步开展勘查工作提供重要的理论依据。The tin deposit area from Longligan is located in the southern margin of the Ruichang-Jiujiang fold fault bundle of Jiujiang Depression in Yangzi Platform and is adjacent to Jiangnan Terrace in the south.The deposit is located on the east side of the Pengshan dome structure and is an important tin deposit in Pengshan tin polymetal-lic ore field in the middle and lower reaches of the Yangtze River.On the basis of previous regional studies,this paper analyzes and summarizes the geological characteristics,ore-controlling factors,and prospecting indicators of the Longligan tin deposit in order to discuss the its origin,so as to further guide the prospecting work of this type of tin deposit in Pengshan area and provide important theoretical basis for the next exploration work in this mine area.

关 键 词：锡矿 地质特征 成因 垄里甘 江西 

分 类 号：P611[天文地球—矿床学]