| 中国板块构造与盐类矿产 |
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| 引用本文： | 关绍曾 江宗龙. 中国板块构造与盐类矿产[J]. 化工矿产地质, 1996, 18(2): 73-81 |
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| 作者姓名： | 关绍曾 江宗龙 |
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| 作者单位： | 化学工业部化学矿产地质研究院 |
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| 摘 要： | 中国大陆的华北、塔里木、准噶尔－兴安、华南及甘青藏等五大板块发展过程中于地块边缘活动带、陆间裂谷、陆内裂谷等场所生成的含盐盆地，沉积了各时期（Ｏ、Ｃ、Ｔ、Ｊ－Ｅ和Ｑ）盐类矿床。通过分析对比认为，甘青藏板块兰坪－思茅拗陷带（Ｊ２－Ｅ１、Ｑ），塔里木板块（Ｃ、Ｋ－Ｅ、Ｑ），华北板块（Ｏ２），华南板块（Ｔ１－２）为成钾有利地带，中国东部众多的Ｋ－Ｅ红层盆地中成钾条件较差
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| 关 键 词： | 中国大陆板块构造 盐类矿产 钾盐 |
CHINESE SALINE DEPOSITS IN RELATION TO PLATE TECTONICS |
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| Guan Shaozeng Jiang Zonglong Wei Dongyan Yang Liuping Xuan Zhiqiang Chen Yancheng Cui Tianxiu Liu Zhenmin Deng Xiaolin Yin Xuemin. CHINESE SALINE DEPOSITS IN RELATION TO PLATE TECTONICS[J]. Geology of Chemical Minerals, 1996, 18(2): 73-81 |
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| Authors: | Guan Shaozeng Jiang Zonglong Wei Dongyan Yang Liuping Xuan Zhiqiang Chen Yancheng Cui Tianxiu Liu Zhenmin Deng Xiaolin Yin Xuemin |
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| Affiliation: | MCI Geological Institute for Chemical Minerals |
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| Abstract: | On the mainland of China there have been five plates: North China, Talimu, Zhungeer Xing’an, South China and Gansu Qinghai Xizang. With their evolutions, large numbers of saline deposits of various ages (O, C, T, J E and Q) took place along the margional mobile belts, intercontinental rifts and intracontinental rifts. Comparative studies suggest that the Lanping Simao depressed belt of Gansu Qinghai Xizang plate(J 2 E 1), Talimu plate (C, K E and Q) and North China plate (O) be regarded as sites favourable for potash deposition but the redbed basins widespreading in East China and aged K E times not. |
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| Keywords: | hinese continental plate plate tectonics saline deposit potash |
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