| 马林诺夫斯基古河谷型铀矿床的地质特征 |
| |
| 引用本文： | 道.,ПС 狄永强.马林诺夫斯基古河谷型铀矿床的地质特征[J].铀矿地质,1996,12(3):135-138. |
| |
| 作者姓名： | 道. ПС 狄永强 |
| |
| 作者单位： | 俄罗斯白桦国营地质企业 |
| |
| 摘 要： | 马林诺夫斯基铀矿床产于西伯利亚地台南西部的中新生代陆相沉积盆地。该盆地为地台型的大型沉积盆地，铀矿床产于盆地东南缘，铀矿化受切割古生代基底的古河谷控制。文中概述了该矿床的地质与矿化特征。
|
| 关 键 词： | 古河谷，地质特征 |
GEOLOGICAL CHARACTERISTICS OF MALINOVSKYPALAEOVALLEY-TYPE URANIUM DEPOSIT |
| |
| B. S. Dolgushin, M. E. Bashenov,E. M. Rubinov, L. E. Zadorin.GEOLOGICAL CHARACTERISTICS OF MALINOVSKYPALAEOVALLEY-TYPE URANIUM DEPOSIT[J].Uranium Geology,1996,12(3):135-138. |
| |
| Authors: | B S Dolgushin M E Bashenov E M Rubinov L E Zadorin |
| |
| Abstract: | Malinovsky uranium deposit is located in a Meso-Cenozoic continental sedimentary basinin the southwestern part of Siberian platform which is a large sedimentary basin of platformtype. The uranium deposit occurs at the southeastern margin of the basin. Uranium mineralization is controlled by the palaeovalley that dissects the palaeozoic basement. This paperbriefly describes the geological and mineralization characteristics of the deposit. |
| |
| Keywords: | Palaeovalley Geological characteristics |
| 本文献已被 CNKI 维普 等数据库收录！ |
