摘要
黔中地区古构造环境对洋水矿区磷矿层的控制作用,经过了很多专家学者的探究,产生了多项研究成果,其中应用了古构造还原模型等方式,模拟还原了古地貌,从而对水下古隆起的控矿作用进行深入研究.该文针对黔中地区古构造环境对洋水矿区磷矿层的控制作用进一步探究,对矿区地质概况、 黔中地区古构造环境详细分析.
The control effect of the paleo-tectonic environment in central Guizhou on the phosphorite deposit in Yangshui mine area has been explored by many experts and scholars,and many research results have been proposed,in which the paleostructure reduction model is applied and the ancient landform is simulated,thus deeply investigating the control effect of palaeohigh.The control effect of paleo-tectonic environment in central Guizhou on the phosphorite deposit in Yangshui mine area is further investigated,and the geological overview of the mine area and the paleo-tectonic environment in the central Guizhou are analyzed in detail.
作者
陈治
Chen Zhi(Geophysical and Geochemical Exploration Institute,Guizhou Bureau of Geology and Mineral Resources,Guiyang 550013,China)
出处
《有色金属设计》
2019年第2期115-117,共3页
Nonferrous Metals Design
关键词
黔中地区
古构造环境
洋水矿区
磷矿层
Central Guizhou area
Paleo-tectonic environment
Yangshui mine area
Phosphorite deposite
