| 四川冕宁尤黑木向形构造解析及控矿模式 |
| |
| 引用本文： | 田作基.四川冕宁尤黑木向形构造解析及控矿模式[J].成都理工大学学报(自然科学版),1997(1). |
| |
| 作者姓名： | 田作基 |
| |
| 作者单位： | 成都理工学院地质学系 |
| |
| 摘 要： | 四川冕宁尤黑木矿区位于扬子地台西缘康滇构造带北段与松潘－甘孜推覆造山带南段接合部的东侧。通过对尤黑木向形的几何结构样式及控矿特征分析，认为铜铁矿体作为相对坚硬岩层，在向形转折端整体构成一钩状褶皱形态，并进一步探讨了其成矿有利地段
|
| 关 键 词： | 向形，钩状褶皱，铜铁多金属矿床，尤黑木 |
THE GENETIC MECHANISM OF YOUHEIMU SYNFORM AND ITS ORE CONTROL CHARACTERISTICS IN MIANNING, SICHUAN |
| |
| Tian Zuoji.THE GENETIC MECHANISM OF YOUHEIMU SYNFORM AND ITS ORE CONTROL CHARACTERISTICS IN MIANNING, SICHUAN[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1997(1). |
| |
| Authors: | Tian Zuoji |
| |
| Institution: | Chengdu University of Technology |
| |
| Abstract: | The Youheimu ore area is located in the western margin of the Yangtze platform. Based on the analysis of structure patterns of the Youheimu synform and ore control characteristics, the Cu and Fe rich sulfide deposits that are competent bed constitute a hookfold form. Finally, the paper puts forward the best part of ore formation. |
| |
| Keywords: | synform hookfold Cu and Fe rich sulfide deposit Youheimu |
| 本文献已被 CNKI 等数据库收录！ |
