| 兰道班江铁矿成矿地质特征及矿床成因 |
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| 引用本文： | 张治中.兰道班江铁矿成矿地质特征及矿床成因[J].吉林地质,2009,28(2):52-55. |
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| 作者姓名： | 张治中 |
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| 作者单位： | 吉林通钢矿业有限责任公司,吉林,长春,130022 |
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| 摘 要： | 通过对马来西亚吉兰丹州兰道班江铁矿地质特征的研究,认为成矿热液来源于中酸性花岗闪长岩体,地层为碳酸盐类,二者发生接触交代作用形成矽卡岩型铁及多金属矿床。
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| 关 键 词： | 铁及多金属矿床 地质特征 兰道班江 马来西亚 |
Geologic features and genesis of Landau Banjiang iron deposit, Kelantan State of Malaysia |
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| ZHANG Zhi-zhong.Geologic features and genesis of Landau Banjiang iron deposit, Kelantan State of Malaysia[J].Jilin Geology,2009,28(2):52-55. |
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| Authors: | ZHANG Zhi-zhong |
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| Institution: | ZHANG Zhi-zhong (Jilin Tonggang Mining Industry Co. , Ltd, Changchun 130022, Jilin, China) |
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| Abstract: | Through the study of geologic features of Landau Banjiang iron deposit,Kelantan,State of Malaysia,it is considered that ore-forming hydrothermal solution derived form neutral and acidic granodiorite,which belongs to carbonate rock.In contact metasomatism,formed skarn type iron and polymetallic ore deposit. |
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| Keywords: | iron and polymetallic ore deposit geologic feature Landau Banjiang Malaysia |
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