| 伊什基里克金矿床地质特征 |
| |
| 引用本文： | 于瑞金.伊什基里克金矿床地质特征[J].矿产与地质,1999,13(6):335-337. |
| |
| 作者姓名： | 于瑞金 |
| |
| 作者单位： | 山东地质勘查局新疆勘查院,滩坊,261021 |
| |
| 摘 要： | 伊什基里克金矿床产于伊犁晚古生代弧间盆地、伊什基里克石炭纪裂陷中的酸性火山碎屑岩地层中，矿体呈脉状，受区域断裂构造控制。矿床的形成与早石炭世火山活动关系密切，提出了中低温火山热液矿床成因的认识。
|
| 关 键 词： | 金矿床 地质特征 成因 伊什基里克 新疆 |
| 文章编号： | 1001-5663(1999)06-0335-03 |
| 修稿时间： | 1999年6月7日 |
STUDYING ON GEOLOGICAL CHARACTERISTICS OF YISHJILIKE GOLD DEPOSIT |
| |
| Yu Ruijin.STUDYING ON GEOLOGICAL CHARACTERISTICS OF YISHJILIKE GOLD DEPOSIT[J].Mineral Resources and Geology,1999,13(6):335-337. |
| |
| Authors: | Yu Ruijin |
| |
| Abstract: | The gold ore deposit is located in acid pyroclastic rock layers of yishijilike fracture, which was formed in Carboniferous period and was lying in yili interarc basin of late Pz. The orebody appears to be vein-type and be controlled by regional fracture. It is believed that the ore deposit is close related with volcanic activity of early carboniferous period in forming process and is of mid-low temperature volcanogene hydrothermal in origin. |
| |
| Keywords: | Gold Deposit Geological characteristics Origin Yishijilike Yili |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
