REE compositions of Lower Ordovician dolomites in Central and North Tarim Basin, NW China: A potential REE proxy for ancient seawater
文献类型：期刊论文
| 作者 | Zhang Xuefeng1; Hu Wenxuan2; Jin Zhijun3; Zhang Juntao2; Qian Yixiong4; Zhu Jingquan5; Zhu Dongya3; Wang Xiaolin2; Xie Xiaomin2 |
| 刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
 |
| 出版日期 | 2008-06-01 |
| 卷号 | 82期号:3页码:610-621 |
| 关键词 | dolomite REE clay contamination Tarim Basin |
| ISSN号 | 1000-9515 |
| 文献子类 | Article |
| 英文摘要 | Rare earth element compositions of Lower Ordovician dolomites in the Central and Northern Tarim Basin are studied. Most dolomite samples are more or less contaminated by clay minerals. Their rare earth element compositions have been consequently changed, showing both seawater-like and non-seawater-like features. The clay contamination should be disposed before the REE data are used. Through ICP-MS and ICP-AES analyses, the REE features are well documented. The clay contamination is quantitatively determined by microscopic investigation, trace elements and REE contents. The dolomites, at least in the Tarim Basin, are thought to he pure when their total LREE contents are less than 3x10(-6). Through comparison, the pure dolomites show similarities in REE patterns but differences in REE contents with co-existing pure limestone, which indicates that dolomitization may slightly change the REE compositions. Nevertheless, whatever the change is, the pure dolomites may act as a potential REE proxy for Ordovician seawater, which would be significant for ancient massive dolomite strata that lack limestone. |
| WOS关键词 | RARE-EARTH-ELEMENTS ; IRON-FORMATIONS ; TRACE-ELEMENTS ; GEOCHEMISTRY ; CARBONATES ; EVOLUTION ; YTTRIUM ; OCEAN ; FRACTIONATION ; FORAMINIFERA |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000258544300015 |
| 出版者 | GEOLOGICAL SOC CHINA |
| 资助机构 | National Basic Research Program(2005CB422103 ; National Basic Research Program(2005CB422103 ; 2005CB422105) ; 2005CB422105) ; National Basic Research Program(2005CB422103 ; National Basic Research Program(2005CB422103 ; 2005CB422105) ; 2005CB422105) ; National Basic Research Program(2005CB422103 ; National Basic Research Program(2005CB422103 ; 2005CB422105) ; 2005CB422105) ; National Basic Research Program(2005CB422103 ; National Basic Research Program(2005CB422103 ; 2005CB422105) ; 2005CB422105) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/69438]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Zhang Xuefeng |
| 作者单位 | 1.China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China 2.Nanjing Univ, State Key Lab Mineral Deposits Res, Nanjing 210093, Peoples R China 3.Petr Explorat & Dev Inst SINOPEC, Beijing 100083, Peoples R China 4.SINOPEC Explorat & Prod Res Inst, Western Branch Inst, Urumqi 830011, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang Xuefeng,Hu Wenxuan,Jin Zhijun,et al. REE compositions of Lower Ordovician dolomites in Central and North Tarim Basin, NW China: A potential REE proxy for ancient seawater[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2008,82(3):610-621. |
| APA | Zhang Xuefeng.,Hu Wenxuan.,Jin Zhijun.,Zhang Juntao.,Qian Yixiong.,...&Xie Xiaomin.(2008).REE compositions of Lower Ordovician dolomites in Central and North Tarim Basin, NW China: A potential REE proxy for ancient seawater.ACTA GEOLOGICA SINICA-ENGLISH EDITION,82(3),610-621. |
| MLA | Zhang Xuefeng,et al."REE compositions of Lower Ordovician dolomites in Central and North Tarim Basin, NW China: A potential REE proxy for ancient seawater".ACTA GEOLOGICA SINICA-ENGLISH EDITION 82.3(2008):610-621. |
入库方式： OAI收割
来源：地质与地球物理研究所
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