|
|||||
|
|
| 从秦皇岛柳江盆地岩浆活动论其大地构造性质及成矿特征 | |
| 引用本文： | 刘锡文. 从秦皇岛柳江盆地岩浆活动论其大地构造性质及成矿特征[J]. 河北理工学院学报, 1995, 0(1) |
| 作者姓名： | 刘锡文 |
| 摘 要： | 秦皇岛柳江盆地自燕山运动以来，岩浆活动十分剧烈，岩浆岩广泛发育，说明它已从稳定区转化为活动区，成为后地台阶段的活化区，即地洼区。因而其成矿作用具有稳定型和治化型两类特征。 |
| 关 键 词： | 岩浆活动，大地构造性质，成矿特征，柳江盆地 |
DISCUSSION OF GEOTECTONIC PROPERTIES AND MINERALIZATION CHARACTERISTICS BASED ON MAGMA IN QINHUANGDAO LIUJIANG BASIN |
|
| Liu Xiwen. DISCUSSION OF GEOTECTONIC PROPERTIES AND MINERALIZATION CHARACTERISTICS BASED ON MAGMA IN QINHUANGDAO LIUJIANG BASIN[J]. Journal of Hebei Institute of Technology, 1995, 0(1) | |
| Authors: | Liu Xiwen |
| Affiliation: | Department of Mining |
| Abstract: | Magma activities in Qinghuangdao Liujiang Basin have been very violent since Yanshanian movement, and Magma rocks are very spread. It demonstrates that Qinghuangdao Liujiang Basin has changed from a steady region into an active region and become the active region of post platforms,that is Diwa region. So its mineralization includes two characteristics which consist of steady type and active type. |
| Keywords: | Magma activity Geotectonic proterty Mineralization characteristies Qinhuangdao Liujiang Basin |
| 本文献已被 CNKI 等数据库收录！ | |