| 中国非金属超大型矿床与板块构造及地壳演化的关系 |
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| 引用本文： | 冉红彦,曹俊臣.中国非金属超大型矿床与板块构造及地壳演化的关系[J].地质与勘探,1996,32(6):1-6. |
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| 作者姓名： | 冉红彦 曹俊臣 |
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| 作者单位： | 中国科学院广州地球化学研究所 |
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| 基金项目： | 国家科技攻关攀登A（30）项目 |
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| 摘 要： | 中国非金属超大型矿床与板构造和地壳演化的关系，表现在不同板块构造环境形成不同的超大型非金属床组合，相同板块构造环境而不同板块对象所形成的超大型非金属矿主档又各有侧重。
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| 关 键 词： | 板块构造 地壳演化 非金属矿床 |
RELATIONSHIP BETWEEN CHINESE SUPER-LARGE NON-METAL DEPOSITS AND PLATE TECTONIC,THE CRUSTAL EVOLUTION |
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| Ran Hongyan,Cao Junchen.RELATIONSHIP BETWEEN CHINESE SUPER-LARGE NON-METAL DEPOSITS AND PLATE TECTONIC,THE CRUSTAL EVOLUTION[J].Geology and Prospecting,1996,32(6):1-6. |
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| Authors: | Ran Hongyan Cao Junchen |
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| Institution: | Ran Hongyan;Cao Junchen |
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| Abstract: | Super-large non-metal deposit assemblage formed in different plate tectonic environment reflected the relationship between Chinese super-large non-metal deposits and plate tectonic,the crustal evolution. Even if in identical plate tectonic environment, super-large non-mdtal deposits produced in different plates would be not alike. In addition,the formation of super-large non-metal deposits such as graphite deposit,phosphorite deposit and diatomite deposit was restricted greatly by the evolution of biosphere,magnesite deposit by the evolution of hydrosphere (paleoseawater). |
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| Keywords: | China super-large non-metal deposits plate tectonic the crustal evolution |
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