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东秦岭地区不仅是我国世界级钼矿的聚集区也是一个重要的金矿和多金属矿聚集区(Mao et al.,2011)。这些矿床主要形成在235~110Ma,且在过去的十年间得到了众多学者的大量研究(Stein et al.,1997;Mao et al.,2002,2011;李永峰等,2005;叶会寿等,2006;Zhang et al.,2007,2011;Chen et al.,2008,2009;Zhu et al.,2009;Xu et al.,2010;
The East Qinling area is not only a gathering area for world-class molybdenum mines in China, but also an important gathering area for gold and polymetallic deposits (Mao et al., 2011). These deposits are mainly formed at 235-110 Ma, and have been extensively studied by many scholars over the past decade (Stein et al., 1997; Mao et al., 2002, 2011; Li Yongfeng et al., 2005; Ye Huishou et al. 2006; Zhang et al., 2007, 2011; Chen et al., 2008, 2009; Zhu et al., 2009; Xu et al., 2010;