| 黄海海州湾钙结体的特征及其地质意义 |
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| 引用本文： | 吴世迎,房泽诚.黄海海州湾钙结体的特征及其地质意义[J].地质科学,1982,0(2):207-214. |
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| 作者姓名： | 吴世迎 房泽诚 |
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| 作者单位： | 国家海洋局第一海洋研究所 |
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| 摘 要： | 近年,我所在黄海底质调查中发现,黄海海州湾海区、成内头海区和渤海海峡海区广泛分布着各种形态的钙结体。为了探明其特征,我们以海州湾海区为例,进行了钙结体的结构、矿物成分、化学成分以及它们的分布状态的研究,并通过海区的地质构造背景、水动力状况、物质通量变化以及生物化学作用等控制因素的分析,对钙结体进行了物质来源和成因上的探讨。
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| 关 键 词： | , |
THE CHARACTERISTICS OF CALICHES IN THE HAIZHOU BAY,HUANGHAI SEA AND ITS GEOLOGICAL IMPLICATIONS |
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| Wu Shiying,Fang Zecheng.THE CHARACTERISTICS OF CALICHES IN THE HAIZHOU BAY,HUANGHAI SEA AND ITS GEOLOGICAL IMPLICATIONS[J].Chinese Journal of Geology,1982,0(2):207-214. |
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| Authors: | Wu Shiying Fang Zecheng |
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| Institution: | First Institute of Oeeanography, National Bureau of Oceanography |
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| Abstract: | The caliches distributed in the Haizhou Bay are in various forms.In order to search for their characteristics in different aspects,great effort has been devoted to the study of texture,mineral composition,chemical composition and distribution pattern.Based on the analysis of main controlling factors,such as geological structure,hydrodynamical feature,change of mass flux and biochemical action etc.,the geological implications of caliches have been discussed. |
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