摘要
钒矿矿床分布于背斜核部,钒矿层赋存于底部假整合于震旦系灯影组(Zbdn)之上的寒武系下统牛蹄塘组下段黑色含炭硅质泥岩系中。在黔北台隆遵义断拱、毕节北东构造变形区及黔中隆起的北缘,背斜核部假整合于震旦系灯影组(Zbdn)之上的寒武系下统牛蹄塘组下段具有极大的找矿前景。
The Ore deposit of vanadium distributes in the back-slope core of Northern Guizhou and the mineral deposit exists in silicon mudstone which contains carbon, from the swelling of Zunyi fractured arch to the transformed regions in the north east of Bijie to the north edge of the central swelling. There is a briUiant prospect of exploring the ore.
出处
《遵义师范学院学报》
2008年第2期98-100,共3页
Journal of Zunyi Normal University
关键词
黔北
钒矿床
地质特征
the north of Guizhou
vanadium deposit
geographical features
