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Zijinshan-bitian Cu-Au-Mo orefield, SW Fujian - An example of gold-rich PCS zoning

机译:Zijinshan-Bitian Cu-Au-Mo orefield,SW福建 - 富含金的PC分区的一个例子

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The Zijinshan-Bitian Cu-Au-Mo orefield is spread to north of the Shanghang County, SW Fujian. In geological structure it is located at the plunging end of NE-trending Xuanhe anticlinorium, in the NE rim of the NW trending Shanghang volcano-sedimentary basin. Orefield basement is composed of the Archean-Middle Proterozoic low-grade metamorphic rock formations, containing marine basic metavolcanic sequenses. Lower Cretaceous subaerial volcanic rocks of andesite-trachy andesite-rhyolite composition fill in the volcano-sedimentary basin.
机译:Zijinshan-Bitian Cu-Au-Mo-Mo orefield蔓延到Sw Fujian的上行县北部。在地质结构中,它位于Ne-Trending Xuanhe Brientlinorium的狭窄端,在NW趋势上行火山沉积盆地的NE rim。厄菲尔德地下室由阿军中间正面的低级变质岩层组成,含有海洋基本的甲状腺序列序列。下白垩纪的胚胎火山岩岩石骨灰碱岩石岩石在火山沉积盆地中填充。

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