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矽卡岩、云英岩、钠长岩和热液类型的矿床是岩浆期后金属矿床的典型代表。到目前为止,相当肯定地确定了这些矿床和其它内生金属矿床成矿物质的来源以及形成这些矿床的矿化热液的来源。成矿物质来源分为:1)壳下玄武岩类的或岩浆的;2)地壳花岗岩类的或同化的;3)渗入的。成矿热水系分力:1)岩浆水;2)交质水; 3)沉积岩的埋藏水;
Skarn, dolostone, albite and hydrothermal deposits are typical representatives of post-magmatic metallogenic deposits. So far, the sources of the metallogenic material for these deposits and other endogenous metallogenic deposits and the sources of mineralized hydrothermal fluids forming these deposits have been fairly well established. The sources of ore-forming materials are divided into: 1) basaltic or magmatic underbodies; 2) the assimilation or assimilation of crustal granites; and 3) infiltration. Mineralization of hot water component: 1) magmatic water; 2) pay the quality of water; 3) sedimentary rock buried water;