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Rare graphic textures of cinnabar-stibnite and cinnabar-chalcopyrite pairs and their genesis

机译:朱砂-闪锌矿和朱砂-黄铜矿对的稀有图形纹理及其成因

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摘要

We consider the rare graphic textures of cinnabar-stibnite and cinnabar-chalcopyrite pairs from the Khaidarkan Sb-Hg deposit (Kyrgyzstan) and the Idermeg-Bayan-Haan-Uul polysulfide-fluorite complex deposit (Mongolia). They resemble the ridge pattern on finger skin. Typical signs suggest the formation of the cinnabar-stibnite graphic texture in two stages of hypogene mineralization: (1) interstitial replacement of granulated stibnite by cinnabar and (2) local recrystallization of combined aggregates during the dynamic metamorphism of the ores with partial migration of substance and the formation of "ordered" graphic textures. This texture is named "the graphic texture of hypogene recrystallization". The formation of the cinnabar-chalcopyrite graphic texture, which has been observed for the first time, is attributed to direct hypogene replacement of cinnabar by chalcopyrite. Chalcopyrite crystallization along the contacts of cinnabar grains is accompanied by the growth of the replacement area. It is proposed to name this texture "the graphic texture of hypogene replacement." The causes of the selective replacement of cinnabar by chalcopyrite, which gave rise to this peculiar texture, remain uncertain.
机译:我们考虑了来自Khaidarkan Sb-Hg矿床(吉尔吉斯斯坦)和Idermeg-Bayan-Haan-Uul多硫化物-萤石复合矿床(蒙古)的朱砂-闪锌矿和朱砂-黄铜矿对的罕见图形纹理。它们类似于手指皮肤上的脊纹。典型迹象表明,在次生矿化的两个阶段中,朱砂-闪锌矿图形纹理的形成:(1)朱砂间隙填充粒状辉石矿;(2)在矿石的动态变质过程中,结合的骨料局部重结晶,且物质发生部分迁移并形成“有序”图形纹理。该纹理被称为“次基因重结晶的图形纹理”。首次观察到的朱砂-黄铜矿图形纹理的形成,归因于黄铜矿对朱砂的直接次基因替代。沿朱砂晶粒接触的黄铜矿结晶伴随着置换区的生长。建议将该纹理命名为“次基因替换的图形纹理”。黄铜矿选择性替代朱砂的原因尚不清楚。

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