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一、前言作者等于1956—1957年在柴达木北緣某鉛鋅矿床氧化带中找到若干含鋅很高的硫酸盐矿物。其中二种,經过1962—63年的室內工作肯定为鋅赤铁矾(Zincobotryogen)和鋅叶綠矾(Zincocopiapite)。前者是赤铁矾族的新变种,后者是叶綠矾族的新变种。它們在成分上接近于这两族矿物的鋅的极端組分,即鋅赤铁矾的理論分子式为ZnFe~(3+)(SO_4)_2(OH)·7H_2O,鋅叶綠矾的理論分子式为ZnFe_4~(3+)(SO_4)_6(OH)_2·2OH_2O。工作中曾利用了叶韵琴同志采集的部分标本。化学分析由地貭部地貭科学院张金叶
I. Preface The author is equal to 1956-1957 in the northern Qaidam a lead-zinc ore oxidation zone to find a number of high zinc sulfate minerals. Two of them, after 1962-63 indoor work, were certainly Zincobotryogen and Zincocopiapite. The former is a new variant of the hematite community, which is a new variant of the phylum. They are close in composition to the extreme components of zinc in these two groups of minerals, ie, the theoretical formula of zinc hematite is ZnFe ~ (3 +) (SO 4) 2 (OH) · 7H 2 O. The theoretical formula of zinc vanadium is ZnFe_4 ~ (3 +) (SO_4) _6 (OH) _2 · 2OH_2O. In the work, some specimens collected by Comrade Ye Yun-qin were used. Chemical analysis by the Department of ground 貭 Academy of Sciences Zhang Jinye