| 湖南片状高岭土矿床成因类型及控矿因素 |
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| 引用本文： | 李洪昌,唐先礼.湖南片状高岭土矿床成因类型及控矿因素[J].湖南地质,1989,8(1):44-50. |
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| 作者姓名： | 李洪昌 唐先礼 |
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| 作者单位： | 湖南省地质矿产局四一七队，湖南省地质矿产局四一七队，湖南省地质矿产局四一七队，湖南省地质矿产局四一七队 |
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| 摘 要： | 湖南片状高岭土矿床丰富多采,按成因可分为两大类五个亚类。不同类型矿床的控矿因素不尽相同。风化残余型片状高岭土矿床主要受母岩、风化程度、地形、地貌等因素的控制。沉积型片状高岭土矿床主要受古地理环境的控制。
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| 关 键 词： | 高岭土矿床 成因类型 挖矿因素 |
GENETIC TYPES AND METALLOGENIC FACTORS OF SCHISTOSE KAOLINITE DEPOSITS IN HUNAN PROVINCE |
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| Li Hongchang Tang Xianli Peng Dingjia Liao Lanmin.GENETIC TYPES AND METALLOGENIC FACTORS OF SCHISTOSE KAOLINITE DEPOSITS IN HUNAN PROVINCE[J].Hunan Geology,1989,8(1):44-50. |
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| Authors: | Li Hongchang Tang Xianli Peng Dingjia Liao Lanmin |
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| Institution: | No.417 Team of Hunan Bureau Geology and Mineral Resources |
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| Abstract: | The Schistose Kaolinite deposits in Hunan are rich and varing in types, Which can be genetically classified into two types and 5 Subtypes. The metallogenic factors are different for different type of deposit. The weathering-residue type is mainly controlled by hostrock, weathering degree, landform and landscape etc; The sedimen tary type is mainly controlled by the paleogeographic enviroments. |
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| Keywords: | kaolinite deposit Genetic type Metallogenic factors Hunan |
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