CHEMICAL-SPECIES OF IRIDIUM AND OTHER TRACE-ELEMENTS AT K-T BOUNDARY CLAY LAYER, STEVNS KLINT, DENMARK, AND ITS IMPLICATION
文献类型:期刊论文
| 作者 | Chai ZF(柴之芳) ; Kong P(孔屏); Mao XY(毛雪瑛); Ma SL(马淑兰); Zhou YQ(周瑶琪); Ma JG(马建国); CHAI, ZF ; KONG, P; MAO, XY; MA, SL
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| 刊名 | SCIENCE IN CHINA SERIES B-CHEMISTRY
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| 出版日期 | 1991 |
| 卷号 | 34期号:12页码:1492-1500 |
| 关键词 | K-T BOUNDARY IR ANOMALY CHEMICAL SPECIES EVENT STRATIGRAPHY |
| 英文摘要 | The chemical species of anomalous Ir in the Fish Clay K-T boundary at Stevns Klint, Denmark, was studied by using a newly-developed chemical stepwise dissolution procedure and neutron activation analysis. The experimental results indicate that the anomalous Ir mostly exists in the acid-insoluble residue phase. The Ir pattern of the K-T boundary resembles that of the Ningqiang carbonaceous chondrite, while remarkably different from those of the ultrabasic rock and volcanic lava. Thus, we deduce that the Ir anomaly at K-T boundary is mainly extraterrestrial, instead of volcanogenic or geochemical enrichment origin. The patterns of other trace elements in various phases also confirm the above conclusion. |
| 学科主题 | Chemistry |
| 类目[WOS] | Chemistry, Multidisciplinary |
| 研究领域[WOS] | Chemistry |
| 原文出处 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:A1991GY89400011 |
| 源URL | [http://ir.ihep.ac.cn/handle/311005/239385] ![]() |
| 专题 | 高能物理研究所_院士 |
| 作者单位 | 中国科学院高能物理研究所 |
| 推荐引用方式 GB/T 7714 | Chai ZF,Kong P,Mao XY,et al. CHEMICAL-SPECIES OF IRIDIUM AND OTHER TRACE-ELEMENTS AT K-T BOUNDARY CLAY LAYER, STEVNS KLINT, DENMARK, AND ITS IMPLICATION[J]. SCIENCE IN CHINA SERIES B-CHEMISTRY,1991,34(12):1492-1500. |
| APA | 柴之芳.,孔屏.,毛雪瑛.,马淑兰.,周瑶琪.,...&MA, JG.(1991).CHEMICAL-SPECIES OF IRIDIUM AND OTHER TRACE-ELEMENTS AT K-T BOUNDARY CLAY LAYER, STEVNS KLINT, DENMARK, AND ITS IMPLICATION.SCIENCE IN CHINA SERIES B-CHEMISTRY,34(12),1492-1500. |
| MLA | 柴之芳,et al."CHEMICAL-SPECIES OF IRIDIUM AND OTHER TRACE-ELEMENTS AT K-T BOUNDARY CLAY LAYER, STEVNS KLINT, DENMARK, AND ITS IMPLICATION".SCIENCE IN CHINA SERIES B-CHEMISTRY 34.12(1991):1492-1500. |
入库方式: OAI收割
来源:高能物理研究所
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