Coarse-grained gold, giant-grained gold and block gold are the common visible in ores.
两矿区的矿石中常见明金，为粗粒金，巨粒金及块状金。
Coarse-crystallized crushing pyrites with high gold content suggest that gold is enriched by tectogenesis.
粗粒破碎的黄铁矿含金较高，说明构造运动使金在黄铁矿中进一步富集。
Mainly coarse grained gold, along with pyrite, pyrrhotite, arsenopyrite, and minor base metal sulfides, occur in networks of quartz veinlets, brecciated wallrock, and disseminated in altered wallrock.
大部分粗粒金主要赋存在网格状石英细脉和角砾状围岩中的黄铁矿、磁黄铁矿、毒砂和少量贱金属硫化物中和以分散状分布在蚀变围岩中。
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