| 磷铁矿(Fe2P)在我国发现 |
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| 引用本文： | 陈克樵,金在淼,彭志忠.磷铁矿(Fe2P)在我国发现[J].地质科学,1983,0(2):199-202. |
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| 作者姓名： | 陈克樵 金在淼 彭志忠 |
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| 作者单位： | 1. 中国地质科学院矿床研究所;2. 金川有色金属公司研究所;3. 武汉地质学院北京研究生部 |
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| 摘 要： | 磷铁矿1)(Fe2.0939Ni0.0746Cr0.0215P发现于我国某地含铂硫化铡镍矿床的原生带中。该矿物是磷铁矿Fe2P-磷镍矿Ni2P系列的端员组分矿物,也是地球上首次发现的一种含铁、磷的金属互化物矿物。
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| 关 键 词： | , |
| 收稿时间： | 1981-04-11 |
| 修稿时间： | 1981-04-11; |
THE DISCOVERY OF IRON BARRINGERITE (Fe2P) IN CHINA |
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| Chen Keqiao,Jin Zaimiao,Peng Zhizhong.THE DISCOVERY OF IRON BARRINGERITE (Fe2P) IN CHINA[J].Chinese Journal of Geology,1983,0(2):199-202. |
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| Authors: | Chen Keqiao Jin Zaimiao Peng Zhizhong |
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| Institution: | 1. Institute Mineral Deposits, Chinese Academy of Geological Science, Beijing;2. Zingchuang Nonferrous Metal Comppany;3. Graduate Department of the Wuhan Geological College, Beijing |
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| Abstract: | Iron Barringerite occurs in the oxidation zone of a certain platinum-bearing copper-nickel sulfide deposit in China.The mineral is near the Fe-end member in the barringerite series and a metallic complementary compound of iron and phosphorus.It was discovered for the first time in terrestrial rocks.Its chemical formula is Fe2P.The mineral is hexagonal with a0=5.857Å and c0=3.452Å;the space group is P62 m.Grain size 0.25?0.1?0.07 mm.VHN20g=1097,anisotropism weak.Reflectances in per cent are as follows. |
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| Keywords: | , |
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