Genesis of the carbonatite-syenite complex and REE deposit at Maoniuping,Sichuan Province, China: Evidence from Pb isotope geochemistry
文献类型：期刊论文
| 作者 | TAO GUAN; CHENG XU; HUAN ZHANG; ZHILONG HUANG; CONGQIANG LIU; WENBO LI; LIANG QI |
| 刊名 | Geochemical Journal
 |
| 出版日期 | 2004 |
| 卷号 | 38期号:1页码:67-76 |
| 关键词 | Genesis Carbonatite Syenite Pb Isotope Maoniuping Ree Deposit |
| 英文摘要 | The Maoniuping REE deposit is the second largest light rare earth elements deposit (1.45 million tons of REE2O3) in China, located in the Panxi rift, Sichuan Province. It is a vein-type deposit hosted within, and genetically related to the Himalayan alkalic carbonatite-syenite complex. The initial 206Pb/204Pb and 208Pb/204Pb ratios from the Maoniuping carbonatites are similar to syenites, which, however, show more radiogenic 207Pb/204Pb ratios. This could not only be attributed to contamination by crustal materials. The Pb-Pb isotope plots from carbonatites and syenites define a linear array between EM1 and EM2. It suggests their sources were located in a heterogeneous lithospheric mantle and produced by the mixture of EM1 with EM2. The initial 206Pb/204Pb and 208Pb/204Pb ratios from fluorites, galenas, pyrites and feldspar are similar to carbonatites and syenites, and different from granites. Their 207Pb/204Pb ratios also plot to between syenites and carbonatites. This suggests the REE ore-forming fluids were derived from carbonatite and syenite magmas. The Pb isotopic results are consistent with a model for REE deposition involving mixing of the F-rich, syenite-derived fluid with Ca-, CO2-bearing fluid evolved from carbonatite magma. The early fluorites have higher 207Pb/204Pb ratio than the later ones, which shows that the REE ore-forming fluids were not contaminated by country rocks fluids. |
| 学科主题 | 矿床地球化学 |
| 语种 | 英语 |
| 公开日期 | 2017-12-19 |
| 源URL | [http://ir.gyig.ac.cn:8080/handle/352002/6797]  |
| 专题 | 地球化学研究所_矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文 |
| 推荐引用方式 GB/T 7714 | TAO GUAN,CHENG XU,HUAN ZHANG,et al. Genesis of the carbonatite-syenite complex and REE deposit at Maoniuping,Sichuan Province, China: Evidence from Pb isotope geochemistry[J]. Geochemical Journal,2004,38(1):67-76. |
| APA | TAO GUAN.,CHENG XU.,HUAN ZHANG.,ZHILONG HUANG.,CONGQIANG LIU.,...&LIANG QI.(2004).Genesis of the carbonatite-syenite complex and REE deposit at Maoniuping,Sichuan Province, China: Evidence from Pb isotope geochemistry.Geochemical Journal,38(1),67-76. |
| MLA | TAO GUAN,et al."Genesis of the carbonatite-syenite complex and REE deposit at Maoniuping,Sichuan Province, China: Evidence from Pb isotope geochemistry".Geochemical Journal 38.1(2004):67-76. |
入库方式： OAI收割
来源：地球化学研究所
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