| 福建浦城中生代铀,多金属矿床形成条件及构造环境分析 |
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| 引用本文： | 聂淦波,隆盛银.福建浦城中生代铀,多金属矿床形成条件及构造环境分析[J].华东地质学院学报,1994,17(2):106-116. |
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| 作者姓名： | 聂淦波 隆盛银 |
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| 摘 要： |
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| 关 键 词： | 多金属矿床 铀矿床 成因 构造环境 |
ANALYSISES ON FORMING CONDITIONS AND TECTONIC SETTING OF MESOZOIC URANIUM,MULTIMETAL ORESIIN PUCHENG OF FUJIAN PROVINCE |
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| Ne Ganbo Rong Shenying Wang Xiaominy.ANALYSISES ON FORMING CONDITIONS AND TECTONIC SETTING OF MESOZOIC URANIUM,MULTIMETAL ORESIIN PUCHENG OF FUJIAN PROVINCE[J].Journal of East China Geological Institute,1994,17(2):106-116. |
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| Authors: | Ne Ganbo Rong Shenying Wang Xiaominy |
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| Institution: | Ne Ganbo Rong Shenying Wang Xiaominy(Editorial Board)(Department of Geoscience)(the Library) |
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| Abstract: | The formation of uranium and multimetal mineral deposits is closely related to the vol-canic activity of late Mesozoic(J_3-K_1)in this area. The mutation zone of the infrastructure and par-tial transverse pullapart position are the best condition of mineral-formation. The volcanic mechanismand explosive breccia pipe overlapped on the ancient metamorphic base and granite are the beneficialspace of ore distribution. Interweaved linear structure is the important factor of controlling volcanicmechanism,ore-body and ore-vein distribution. Deep materials are the main source of materials in min-eral-formation. |
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| Keywords: | uranium deposits5 polymetallic deposits volcanic mechanism zexplosivce breccia pipes5 Fujian Pucheng |
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