| 张园,万梦,欧阳学财,杨立飞.江西垄里甘锡多金属矿地质特征及矿床成因分析[J].矿产勘查,2024,15(S2):425-431 |
| 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 |
| 投稿时间：2024-06-11 |
| DOI：10.20008/j.kckc.2024s2058 |
| 中文关键词: 锡矿 地质特征 成因 垄里甘 江西 |
| 英文关键词: tin ore geological characteristics genesis Longligan Jiangxi Province |
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| 中文摘要: |
| 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。 |
| 英文摘要: |
| The tin deposit area from Longligan is located in the southern margin of the Ruichang -Jiujiang foldfault bundle of Jiujiang Depression in Yangzi Platform and is adjacent to Jiangnan Terrace in the south. The depositis 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 oftin deposit in Pengshan area and provide important theoretical basis for the next exploration work in this mine area. |
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