| 浅谈阿舍勒黄铁矿型多金属矿的垂直分带 |
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| 引用本文： | 陈文鳌,赵云长,吴长江. 浅谈阿舍勒黄铁矿型多金属矿的垂直分带[J]. 新疆地质, 1989, 0(1) |
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| 作者姓名： | 陈文鳌 赵云长 吴长江 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第四地质大队(陈文鳌，赵云长)，新疆维吾尔自治区地质矿产局第四地质大队(吴长江) |
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| 摘 要： | 阿舍勒黄铁型多金属矿床位于阿尔泰地槽褶皱系的中泥盆统安山质—英安质火山—沉积岩中.矿体充填在火山管道内或火山口近侧,主矿体隐伏地下.矿化元素有铁、铜、铅、锌、金、银、硫、钡等,伴生有锗、镓、铟、硒、镉、铋等.矿体上部形态复杂并有分枝,向深部连成一体,是一个向北东侧伏的筒状体.矿体自上而下具垂宜分带,依次为:重晶石—硅化带;黄铁矿—多金属带;黄铁矿—铜、锌带等…
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| 关 键 词： | 重晶石—硅化带 黄铁矿—多金属带 黄铁矿—铜锌带等 中泥盆安山质—英安质火山—沉积岩 阿尔泰地槽褶皱带 |
A PRELIMINARY DISCUSSION OF THE VERTICAL ZONATION ON THE PYRITE POLYMETALLIC DEPOSIT IN ASHELE |
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| Chen Wenao Zhao Yunchang Wu Changjiang. A PRELIMINARY DISCUSSION OF THE VERTICAL ZONATION ON THE PYRITE POLYMETALLIC DEPOSIT IN ASHELE[J]. Xinjiang Geology, 1989, 0(1) |
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| Authors: | Chen Wenao Zhao Yunchang Wu Changjiang |
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| Abstract: | The polymetallic deposit of Ashele pyrite type is contributed in middle Devonian quartz-andesitic volcanosedimentary series in Altai geosyncline fold system.The ore is filled in the volcanic vent or round the crater with the major body buried underground. The ore-forming elements are iron, copper, lead, zink. gold, silver, sulfer, barium etc, with the accompanying elements being germanium, gallium, indium, selenium, cadmium bismuth etc.Morphologically the ore body is complex and branching off in its upper part, but unified in the depth. It is a tubular body tipping east and tilting north.The vertical zonation is noticed in the ore body from up to down as follows:1. barite-silicification zone;2. pyrite-polymetallic zone:3. pyrite-copper, zink zone; |
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| Keywords: | barite-silicification zone pyrite-polymetallic zone pyrite-copper zink zone etc middle Devonian quartz-andesitic volcanosedimentary series Altai geosyncline fold system |
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