| 论风化壳相、古风化壳相矿床 |
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| 引用本文： | 廖士范.论风化壳相、古风化壳相矿床[J].沉积与特提斯地质,1992,12(1):11-19. |
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| 作者姓名： | 廖士范 |
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| 作者单位： | 贵州省地矿局 |
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| 摘 要： | 一、导论现代风化作用形成的风化壳相矿床和更新世以前古风化作用形成的古风化壳相矿床,既不同于一般陆相沉积,如河流相、湖沼相沉积,也不同于一般海相沉积。它们有大同小异的形成机制和物质组成,后者包括风化壳物质的结构、构造,如碎屑、砾块,豆鲕、结核(结石)及矿物组成。它们都是现代风化作用或古风化作用形成的,不是水体中沉积的
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DISCUSSIONS ON THE MODERN AND ANCIENT WEATHERING CRUST DEPOSITS |
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| Liao Shifan.DISCUSSIONS ON THE MODERN AND ANCIENT WEATHERING CRUST DEPOSITS[J].Sedimentary Geology and Tethyan Geology,1992,12(1):11-19. |
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| Authors: | Liao Shifan |
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| Institution: | Guizhou Bureau of Geology and Mineral Resources |
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| Abstract: | It is suggested that both the weathering crust deposits resulted from modern weathering processes and the ancient weathering crust deposits resulted from pre-Pleistocene weathering processes differ from the general continental sediments and common marine sediments, respectively. They are well worth discussing as a kind of characteristic rock facies. |
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