Dongchuang Pb Au deposit is a large quartz vein type deposit.
东闯铅、金矿床是一大型石英脉型矿床。
The later stage of mineralization is of ductile-brittle shearing and brittle shearing, which formed cataclastic quartz-vein type Au deposit.
晚期形成碎裂石英脉型金矿、属韧-脆性和脆性成矿期。
The later stage of mineralization is of ductile-brittle shearing and brittle shearing, which formed cataclastic quartz-vein type Au deposit.
晚期形成碎裂石英脉型金矿、属韧-脆性和脆性成矿期。
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