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Unusual secondary copper assemblages from deposits in eastern Australia

机译:澳大利亚东部矿床中异常的次级铜组合

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Recent open-cut mining operations associated with Cu and Cu-Au orebodies in eastern Australia have revealed a number of exotic assemblages of secondary minerals. The cases examined here all feature secondary phosphates or arsenates and other rather rare species; each of them is noteworthy in terms of the abundance of material that has been recovered. In the Northparkes E22 and E27 deposits at Goonumbla, New South Wales, upper oxidation zones are dominated by libethenite and pseudomalachite, with azurite and malachite emplacement at greater depths. In the nearby E26 deposit, oxidation associated with much more saline (NaCl) ground waters has led to extensive development of sampleite in the phosphate assemblage. Lower in the profile much atacamite was present. A similar pattern of zoning is associated with the oxidized zone of the Girilambone mine, at Girilambone, New South Wales, Secondary copper phosphates were encountered at all levels of the oxidized zone but were particularly pronounced in the upper benches. Deeper in the profile, abundant crystalline native copper was encountered, together with magnificent groups of azurite crystals. Related secondary copper arsenates conspicuous in a paragenetically early sequence of the oxidized zone of the New Cobar mine, Cobar, New South Wales. Associated phases were bayldonite, duftite, gartrellite, agardite, mimetite and various arsenic-bearing members of the jarosite supergroup. A later carbonate sequence (azurite-malachite) was superimposed on this assemblage.
机译:最近在澳大利亚东部,与铜和铜金矿体有关的露天开采活动显示出许多次要矿物的奇特组合。此处检查的病例均具有二次磷酸盐或砷酸盐以及其他相当稀有的物种。就回收的丰富材料而言,它们中的每一个都是值得注意的。在新南威尔士州Goonumbla的Northparkes E22和E27矿床中,上部氧化带主要是白铁矿和假孔雀石,而石棉和孔雀石的埋入深度更大。在附近的E26矿床中,与更多的盐水(NaCl)地下水相关的氧化导致磷酸盐组合物中的磷矿大量开发。在轮廓较低的位置,存在许多方石沸石。在新南威尔士州的吉里拉姆邦,吉里拉姆博恩矿区的氧化带也有类似的分区模式。在氧化层的所有水平都遇到了磷酸二氢铜,但在上层台架中尤为明显。在剖面的更深处,遇到了丰富的结晶天然铜,以及宏伟的蓝铜矿晶体群。相关的次生铜砷在新南威尔士州新巴尔市新巴尔镇矿的氧化带的偏磁地层早期序列中显着。伴生相为黄钾铁矿超群的钠铝矾,榴辉岩、,榴石,辉绿岩,闪锌矿和各种含砷成员。后来的碳酸盐序列(金石-孔雀石)被叠加在该组合上。

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