| 青海省元石山铁镍矿床铁镍元素的赋存状态及变化规律 |
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| 引用本文： | 刘福祥,于家明,赵坤,崔明洙.青海省元石山铁镍矿床铁镍元素的赋存状态及变化规律[J].吉林地质,2007,26(2):27-31. |
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| 作者姓名： | 刘福祥 于家明 赵坤 崔明洙 |
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| 作者单位： | 1. 吉林省第五地质调查所,吉林,九台,130500
2. 吉林省第六地质调查所,吉林,延吉,133001 |
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| 摘 要： | 青海省元石山铁镍矿床产于超基性岩体中,其成矿元素赋存状态与典型的岩浆型矿床有很大差别。成矿元素N i不以独立矿物形式存在,而是呈氧化态被铁吸附成凝胶状态存在。本文主要对矿床成矿元素及伴生有益元素的赋存状态及变化规律进行归纳总结。
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| 关 键 词： | 铁镍矿床 赋存状态 氧化态 凝胶状态 青海省元石山 |
| 文章编号： | 1001-2427（2007）02-027-05 |
| 收稿时间： | 2006-12-15 |
| 修稿时间： | 2007-04-14 |
The occurrence state and changing regularity of the Yuanshishan awaruite deposit, Qinghai Province |
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| LIU Fu-xiang,YU Jia-ming,ZHAO Kun,CUI Ming-zhu.The occurrence state and changing regularity of the Yuanshishan awaruite deposit, Qinghai Province[J].Jilin Geology,2007,26(2):27-31. |
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| Authors: | LIU Fu-xiang YU Jia-ming ZHAO Kun CUI Ming-zhu |
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| Institution: | 1. The Fifth Geologic Survey of Jilin Province, Jiutai 130500, China; 2. The Sixth Geologic Survey of Jilin Province, Yanji 133001, China |
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| Abstract: | The Yuanshishan awaruite deposit,Qinghai Province,is occurred in the ultrobasic rock bodies,the occurrence state of the metallogenic elements has larger difference with the type magmatic deposit.The metallogenic element Ni shows oxidized jelly-like state is adsorbed by iron,and not independent mineral state.In this paper,the metallogenic elements,the occurrence state of the useful associated elements and its changing regularity are mainly reduced and summed up. |
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| Keywords: | awaruite deposit occurrence state oxidized state jelly-like state Yuanshishan of Qinghai Province |
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