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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Magmatic sequences in the Halasu Cu Belt, NW China: Trigger for the Paleozoic porphyry Cu mineralization in the Chinese Altay-East Junggar
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Magmatic sequences in the Halasu Cu Belt, NW China: Trigger for the Paleozoic porphyry Cu mineralization in the Chinese Altay-East Junggar

机译:中国西北地区哈拉苏铜矿带的岩浆层序:中国阿尔泰东部准gar尔古生代斑岩铜矿化的触发条件

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摘要

The Halasu porphyry copper belt situated in the East Junggar is one of the major porphyry copper belts in Xinjiang Uygur Autonomous Region, northwest China. Copper and molybdenum mineralization occurs as disseminated sulfides or veinlets mainly in granodiorite porphyry and diorite porphyry, with the intense development of zoned alteration from potassic, through sericitic to an outer zone of propylitic alteration.
机译:位于准Jung尔东部的哈拉苏斑岩铜带是中国西北维吾尔自治区的主要斑岩铜带之一。铜和钼矿化主要是在花岗闪长斑岩和闪长斑状斑岩中以弥散的硫化物或脉状形式出现,随着钾化,浆液化到丙二酸化变质外部区域的区域性变化而强烈发展。

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