ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鄂西台地东部陡山沱期微生物泥丘的聚磷控矿作用
  
关键词:east region of western Hubei platform  mud mounds  biocenosis  phosphate-rich
基金项目:国家自然科学基金,地质行业基金
作者单位
陈辉能 中国地质科学院天津地质矿产研究所 
朱士兴 中国地质科学院天津地质矿产研究所 
管爱莲 中国地质科学院天津地质矿产研究所 
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摘要:
Control of Phosphate Accumulation in Microlial Mud-Mounds of the Doushantuo on Stage in East Part of the Western Hubei Platform
      The Sinian Period of the Doushantuo an stage in the east region of Western Hubei Platform is an important place forming major phosphorite deposits in China. In the phosphate bearing horizons of the Doushantuo Formation, various kinds of mud mounds are vastly developed in this plotform, especially in its eastern portion. The mud mounds contain in phosphatic deposits and control the shape and grad of the phosphorite deposits. The present research indicates that the supersession of microbial communities restrained the adulteration of carbonates when the phosphates were deposited in sea water,while ancient ecological environments changed from benthic microbial communities in clean water to planctonic ones respectively in clim water and turbid weter. Tree types of phosphatic mud mounds (i.e.Types Ⅰ, Ⅱ and Ⅲ) were formed and they generated the main phosphorite deposits utilized by industry in this area.
CHEN Hui-neng,ZHU Shi-xing,GUAN Ai-lian.1998.Control of Phosphate Accumulation in Microlial Mud-Mounds of the Doushantuo on Stage in East Part of the Western Hubei Platform[J].Acta Geoscientica Sinica,19(3):261-270.
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