抚顺南口前中生代花岗岩是重熔型花岗岩，成岩物质源自深部地壳。
The granite of Mesozoic in Nankou-qian of Fushun is a remelting one, mainly from the deep part of the earth's crust.
南口前一带金矿床的稳定同位素研究表明，金矿成矿与太古宙花岗岩—绿岩带，南口前花岗岩体关系密切。
Studies on stable isotopes in gold deposits in Nankouqian area show that the geneses of the gold deposits are closely related to the Archean granite-greenstone belt.
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