摘要
综述了硅酸盐溶解、砂岩溶蚀的研究成果,指出了此种作用在矿产形成和储集中的重要意义;还论述了表生带中碳酸盐矿物和硅酸矿物的溶解作用及其在成长和植物营养中的意义。
It summarizes the studying achievement of the silicate dissolution and sandstone, and then points out the important significance in the formation and reservoir of the mineral. In this article, it also discusses the solution of carbonate mineral and silicate mineral in the hypergene zone and its significance in the growing and the plant nutrition.
出处
《贵州地质》
2008年第1期51-58,共8页
Guizhou Geology
