文件名称:Finite element modeling of pore-fluid flow in the Dachang ore district, Guangxi, China: Implications for hydrothermal mineralization (2011年)
文件大小:6.9MB
文件格式:PDF
更新时间:2024-05-31 15:39:30
自然科学 论文
Convective heat transfer associated with the circulation of pore-fluid in porous rocks and fractures within the upper crust of the Earth is substantial when the temperature gradient is sufficiently high. In order to understand the process of Sn-polymetall