摘要
金渠金矿区位于小秦岭金矿田中东部。本文通过对该矿床中303和202两条重要矿脉的稳定同位素(S,O,H,C和Pb)组成和成矿物理化学条件等方面的研究,结合以往科研成果,探讨金渠金矿区矿床成因及成矿机制。
Jinqu gold deposit is located in the middle portion of the Xiaoqingling goldfield. Based on recent studies of the compositions of stable isotopes (S, O , H, C and Pb) and ore-forming physiochemical conditions of two important veins (303 and 202) occurred within the deposit, in combination with previous relevant works, the genesis and ore-forming mechanism of the deposit are discussed.
出处
《黄金科学技术》
2004年第2期22-26,共5页
Gold Science and Technology
