| 何财福,张晓娟,范彦慧.青海坑得弄舍金多金属矿床特征及控矿因素[J].矿产勘查,2012,3(6):790-794 |
| 青海坑得弄舍金多金属矿床特征及控矿因素 |
| Deposit characteristics and analysis on ore-controlling factors of Kengdenongshe gold polymetallic deposit, Qinghai |
| 投稿时间：2011-12-28 |
| DOI： |
| 中文关键词: 化探异常 坑得弄舍 重晶石型金多金属矿 控矿因素 青海 |
| 英文关键词: Kengdenongshe geochemical anomaly barite-type gold-polymetallic deposit ore-controlling factors Qinghai |
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| 中文摘要: |
| 坑得弄舍矿床是青海省有色地质矿产勘查局近几年在青海果洛地区新发现的典型金铅锌多金属矿床,该矿床以受岩性层位控制明显、延伸稳定、规模较大及找矿前景明朗为特点,经初步研究认为其成矿类型为喷流沉积—叠加热液改造型。随进一步地质勘探工作的开展,有望成为大型金铅锌多金属矿床。 |
| 英文摘要: |
| Kengdenongshe gold deposit is the typical gold lead-zinc polymetallic deposit discovered by Qinghai Bureau of Nonferrous Metals Exploration recently in Guoluo District, Qinghai Province,the deposit is charactered with the apparent host lithological layers, stable extentionand large size and potential prospecting;Based on the preliminary studies, the authors conclude that the deposit is originated from the sedimentary exhalative deposition and reformed by the laterhydrothermal mineralization.There is a great potential for discovering a large sized gold-lead-zinc polymetallic deposit by the further geological exploration. |
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