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The bio-barite in witherite deposits from Southern Qinling and its;significance
Lu, ZC3; Liu, CQ; Liu, JJ; Wu, FC
刊名PROGRESS IN NATURAL SCIENCE
2004
卷号14期号:10页码:889-+
关键词bio-barite carbon and oxygen isotopes early diagenesis witherite deposits
ISSN号1002-0071
DOI10.1080/10020070412331344511
英文摘要Being stratiform or stratoid, the Huangboshuwan witherite deposit at Zhiyang and the Wenyuhe witherite-barite deposit at Zhushan occur in the lower Lower Cambrian siliceous rocks and the orebodies are remarkably controlled by lithological character and petrography. Carbon and oxygen isotopic studies of witherite, barytocalcite and calcite have shown that the carbon, involved in the formation of these minerals, was derived largely from organic carbon resultant from degradation, polycondensation and dehydroxylation of bio-organic matter in sediments at the early stage of diagenesis. Extensive occurrence of bio-barite strongly evidenced that Ba2+ was concentrated and settled down in the form of bio-barite on the seafloor as a result of biological processes, thereafter forming the initially enriched orebodies of barium deposits. The witherite was metasomatic products of bio-barite under the action of sulfate-reducing bacteria and organic and inorganic reduction.
学科主题矿床地质
WOS研究方向Materials Science ; Science & Technology - Other Topics
语种英语
出版者TAYLOR & FRANCIS LTD
WOS记录号WOS:000224688400009
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/37667]  
专题中国地质调查局
作者单位1.China Geol Survey, Ctr Res & Dev, Beijing 100037, Peoples R China.
2.Chinese Acad Sci, Inst Geochem, Guiyang 550002, Peoples R China.
3.中国地质调查局发展研究中心
推荐引用方式
GB/T 7714
Lu, ZC,Liu, CQ,Liu, JJ,et al. The bio-barite in witherite deposits from Southern Qinling and its;significance[J]. PROGRESS IN NATURAL SCIENCE,2004,14(10):889-+.
APA Lu, ZC,Liu, CQ,Liu, JJ,&Wu, FC.(2004).The bio-barite in witherite deposits from Southern Qinling and its;significance.PROGRESS IN NATURAL SCIENCE,14(10),889-+.
MLA Lu, ZC,et al."The bio-barite in witherite deposits from Southern Qinling and its;significance".PROGRESS IN NATURAL SCIENCE 14.10(2004):889-+.
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