摘要
广西白石普查区锡矿构造位置上位于桂北隆起九万大山褶断带,代表断裂有四堡—天河断裂和池洞断裂,北东向的次生小断裂是重要的导矿容矿构造,锡矿体主要赋存于中细粒二云母花岗岩体内的构造蚀变带中。通过对普查区地质特征、控矿因素、矿床成因的研究,认为矿体深部和北东向断裂带延伸区域具有较大的找矿潜力,建议下一步开展详细的地、物、化、遥综合找矿工作和成矿预测,这将是对寻找新资源突破具有重要的意义。
There are more and more geological workers' attention In the area of baishi census in GuangXi Province.Through the study of the geological characteristics, the controlling factors and the causes of the deposit in the census area.It is believed that the deep part of the mineral body and the extended area of North east to the fault zone have great potential for prospecting. This will be important significance for the search of tin ore resources breakthroughs.
出处
《世界有色金属》
2017年第17期87-89,共3页
World Nonferrous Metals
基金
广西科技计划项目"桂林理工大学地质博物馆科普示范基地建设"(课题编号:桂科AD16450001)研究成果之一
关键词
白石普查区
锡矿
地质特征
找矿前景
Baishi census area
Tin mineral
Geological characteristics
The prospect of mineral