中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Platinum group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province, SW China

文献类型:期刊论文

作者Liang Qi;Mei-Fu Zhou
刊名Chemical Geology
出版日期2008
卷号248页码:83–103
关键词Basalts Pge Re–os Isotopes Emeishan Continental Flood Basalts Sw China
英文摘要

The 260 Ma Emeishan continental flood basalts (ECFB) occur in SW China and northern Vietnam. A 550-m-thick sequence of ECFB in Guizhou Province (SW China) is composed of 12 basaltic lava flows, each ranging from 10 to 140 m in thickness. All samples belong to the high-Ti basalts (TiO2 = 1.9–4.4 wt.% and Ti/Y = 400–700). Relative to the upper flows (Flows 9–12), those from the lower part of the section (Flows 1–8) are depleted in Nb, Ta, P and Sr and enriched in Zr, La and Th, consistent with higher degree of crustal contamination. Overall, the concentrations of Os, Ir and Ru range from 0.01 to 0.23 ppb and are low relative to those of Rh, Pt and Pd, which range from 0.2 to 1.1, 6 to 17 and 5 to 18 ppb, respectively. Different lava flows have different primitive mantle-normalized PGE patterns, and samples from the same flow show similar patterns. Fractionations between PPGE and IPGE are mainly controlled by olivine and chromite fractionation. The negative correlations between Pd/Ir and Pt/Pd, and Ni/Pd and Pd/Cr are consistent with crystal fractionation. Flows 6–8 and 10–12 show obvious negative Ru anomalies, explained by fractionation of laurite (Ru, Os, Ir)S2 or Os–Ir–Ru alloys in the primary magma, or by coprecipitation of laurite with chromite or olivine. Flows 9–12 are Os-poor and have higher initial 187Os/188Os ratios than Flows 1–8, indicating it is easy to alter the Os isotopic compositions of basaltic magmas with lower Os concentrations.

语种英语
源URL[http://ir.gyig.ac.cn/handle/42920512-1/8111]  
专题地球化学研究所_矿床地球化学国家重点实验室
作者单位1.Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, China
2.State Key Lab of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002, China
推荐引用方式
GB/T 7714
Liang Qi;Mei-Fu Zhou. Platinum group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province, SW China[J]. Chemical Geology,2008,248:83–103.
APA Liang Qi;Mei-Fu Zhou.(2008).Platinum group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province, SW China.Chemical Geology,248,83–103.
MLA Liang Qi;Mei-Fu Zhou."Platinum group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province, SW China".Chemical Geology 248(2008):83–103.

入库方式: OAI收割

来源:地球化学研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。