| 吉林省珲春市黄松甸子砾岩型金矿床地质特征 |
| |
| 引用本文： | 刘宝成,袁力.吉林省珲春市黄松甸子砾岩型金矿床地质特征[J].吉林地质,1994,13(1):69-79. |
| |
| 作者姓名： | 刘宝成 袁力 |
| |
| 作者单位： | 吉林省地矿局第六地质调查所 |
| |
| 摘 要： | 黄松甸子砾岩型金矿床位于中新生代滨太平洋活动带，长白－春化裂谷的北端春化盆地内。矿体赋存于第三纪冲洪积层底部粗碎屑沉积中，为一河流冲积扇沉积矿床。成矿物质来原为中性－中酸性岩类及赋存于其中的热液脉金矿化体。重砂矿物除自然金外还见有３０余种其它矿物，并伴生可供综合利用的有益矿物钛铁矿和锆石。
|
| 关 键 词： | 金矿床 地质特征 砾岩型 |
THE GEOLOGICAL FEATURES OF CONGLOMERATE TYPE GOLD DEPOSIT IN HUANGSONGDIANZI,HUNCHUN CITY,JILINPROVINCE |
| |
| Liu Baocheng Yuan Li.THE GEOLOGICAL FEATURES OF CONGLOMERATE TYPE GOLD DEPOSIT IN HUANGSONGDIANZI,HUNCHUN CITY,JILINPROVINCE[J].Jilin Geology,1994,13(1):69-79. |
| |
| Authors: | Liu Baocheng Yuan Li |
| |
| Abstract: | The Huangsongdianzi conglomerate type gold deposit is located in the Northern Chun-hua Basin of the Changbai-Chunhua rift of the Meso-Cenozoic marginal-Pacific active belt.The metal-logenic belt is located in the eastern part of the Wufeng-Ciweigou-Xiaoxinanchagold-copper me tallogenic belt. The orebody occurred in the basal clastic sediments of theTertiary alluvial-pluvial deposit belonging to a river fan sedimentary mineral deposit. Theore-forming elements are derived from the intermediate and intermediate-acid rocks whichcontain hydrothermal vein gold except for native gold,there are more than 30 kinds of miner-als associated wity ilmenites and zircons. |
| |
| Keywords: | Huangsongdianzi Conglomerate type gold deposit River alluvial fan |
| 本文献已被 CNKI 维普 等数据库收录！ |
