| 双桥大断裂带之基本特征及其与铀矿的关系 |
| |
| 引用本文： | 杨顺田.双桥大断裂带之基本特征及其与铀矿的关系[J].浙江国土资源,1995(2). |
| |
| 作者姓名： | 杨顺田 |
| |
| 作者单位： | 华东地质勘探局二六九大队!金华，321028 |
| |
| 摘 要： | 本文通过双桥大断裂带区域地质背景的描述，断裂带基本特征的分析及其对铀矿化的控制作用的综合研究。作为浙江中西部一条区域性大断裂一部分的双桥大断裂带，其活动时间长，结构面复杂，多次活动的特点，它不仅控制岩石的分布，还起到了铀元素储集成矿的控制作用。使铀矿化带、铀矿床及铀矿体在空间展布的一致性和在成矿时间上、成因上的统一性。它对指导找矿、勘探和开采同具重要的现实地质意义。
|
| 关 键 词： | 双桥大断裂带 基本特征 控制作用 地质意义 浙江中西部 |
THE BAISC FEATURES OF SHUANGQIAO LARGE FAULT AND ITS RELATION TO URANIUM MINERALIZATION |
| |
| Authors: | Yang Shuntian |
| |
| Abstract: | Shuangqiao large fault is a part of the regional large fault in mid-west of Zhejiang. It has such features as long time of activity,complicated structural plane and sereral times of activities. In addition,it not only contros the distribution of rocks,but also controls the concentration of uranium. The fault made the uranium mineralization belts,uranium deposits and uranium orebodies concordant in spatial distribution,and united in mineralization period and genesis. It is significant in prospecting,exploration and mining of uranium deposits. |
| |
| Keywords: | Shuangqiao large fault basic features control geological significance |
| 本文献已被 CNKI 等数据库收录！ |
