| 海州式磷矿床成矿模式 |
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| 引用本文： | 熊先孝,姚超美,黄巧. 海州式磷矿床成矿模式[J]. 南方国土资源, 1998, 0(1) |
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| 作者姓名： | 熊先孝 姚超美 黄巧 |
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| 作者单位： | 化工部化学矿产地质研究院，广西地质矿产厅 |
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| 摘 要： | 磷元素在地壳发展过程中，随磷矿成矿作用不同阶段物化条件改变而变化。将成矿划分为沉积、变质及改造三阶段。成矿时代为中元古代早期。由沉积、变质、混合岩化交代和风化淋滤作用，使磷质活化，在一定空间富集成矿。
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| 关 键 词： | 磷矿床 成矿模式 海州式 |
MINERALIZATION MODEL OF HAIZHOU-TYPE PHOSPHIDE DEPOSIT |
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| Xiong Xianxiao , Yao Chaomei. MINERALIZATION MODEL OF HAIZHOU-TYPE PHOSPHIDE DEPOSIT[J]. land and resources of southern china, 1998, 0(1) |
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| Authors: | Xiong Xianxiao & Yao Chaomei |
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| Abstract: | In the development procedure of the crust, the element phosphorus varies in pace with the change of physical and chemical conditions in the different phases of phosphoric mineralization. Its mineralization can be divided into three phases, deposition phase, metamorphism phase and reformation phase. The mineralization epoch is the early period of mesoproterozoic Era. Due to the deposition, metamorphism, migmatization and weathering infiltration, phosphoric substances are remobilized, concentrating and mineralizing in a certain space. |
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| Keywords: | phosphide deposit mineralization model Haizhou-type. |
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