| 云南东川岔河铁矿成因探讨 |
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| 引用本文： | 黄学军,何寿益.云南东川岔河铁矿成因探讨[J].云南地质,2013(4):400-401,385. |
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| 作者姓名： | 黄学军 何寿益 |
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| 作者单位： | [1]香格里拉县云矿红牛矿业有限公司,云南迪庆674400 [2]昆明天骞矿产资源咨询服务有限公司,云南昆明650224 |
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| 摘 要： | 岔河铁矿产于构造破碎带中,似层状产出,围岩和矿体中石英、方解石脉发育,矿床成因属浅海一滨海相沉积变质型褐铁矿床.
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| 关 键 词： | 沉积—变质褐铁矿 层控明显 后期变质 下元古界通安组 云南东川岔河 |
A DISCUSSION ABOUT THE GENESIS OF CHAHE FE DEPOSIT IN DONGCHUAN,YUNNAN |
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| Institution: | HUANG Xue-jun, HE Sou-yi ( 1. Yunkuang Hongniu Mining Company (2. KunmingTianqian Consulting Service Company ( Ltd) of Xianggelila, Diqing 674400) (Ltd) of Mineral Resources, Kunming 650224) |
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| Abstract: | Chahe Fe deposit is in the structural fracture zone, and in stratoid occurrence. The quartz and calcite veins are developed in the wall rock and ore body. It is a sedimentary metamorphic limonite deposit of epicontinental - littoral facies in genesis. |
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| Keywords: | Sedimentary Metamorphic Limonite Deposit Clear Stratabound Posterior Metamorphism Lower Proterozoic Tongan Formation Chahe Dongchuan Yunnan |
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