首页> 外文期刊>Indian journal of geology >GOLD MINERALISATION IN RED SEA HILLS REGION, APART OF SAHARA DESERT, NORTHEAST SUDAN
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GOLD MINERALISATION IN RED SEA HILLS REGION, APART OF SAHARA DESERT, NORTHEAST SUDAN

机译:苏丹东北部撒哈拉沙漠APART红海山地区的金矿化

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摘要

In Sudan gold occurrences are mainly concentrated in Red Sea Hills region. Northeastern part of the country. Most of the gold occurrences in this region were superficially exploited in Pharaonic times as evidenced by old workings & numerous millstones. The gold mineralization in different parts of Red Sea Hills region are mainly associated with quartz veins & alteration zones confined within metavolcanics & meta-sedimentary rocks of Proterozoic age. These rocks have been subjected to low grade greenschist facies metamorphism. The gossan type deposit is characterised by a carbonate sedimentary complex intersected by gabbroic bodies. The gossan has been affected by regional metamorphism. The gold mineralization is intimately associated with ferruginous facies.
机译:在苏丹,金矿主要集中在红海山地区。该国的东北地区。该地区的大部分金矿在法老时期就被浅层开采,这由古老的工艺和无数的磨石证明。红海山地区不同地区的金矿化主要与石英脉和蚀变带有关,这些石英脉和蚀变带局限于元古代的变火山岩和准沉积岩中。这些岩石已经经历了低品位的绿片岩相变质作用。戈桑型沉积物的特征是碳酸盐岩沉积复合物与辉长岩体相交。戈桑已经受到区域变质的影响。金矿化与铁质相密切相关。

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