Geochemistry of the lava and its implications in Musicians Seamounts | |
Li Chuanshun1,2; Pan Yucheng3; Li Anchun1; Batiza, Rodey3 | |
刊名 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY |
2008-11-01 | |
卷号 | 26期号:4页码:459-468 |
关键词 | Musicians Seamounts Geochemistry Hotspot Mid-ocean Ridge Ridge-hotspot Interaction |
ISSN号 | 0254-4059 |
DOI | 10.1007/s00343-008-0459-8 |
文献子类 | Article |
英文摘要 | Chemical and isotopic data of the lava samples dredged in the southern Bach Ridge and the northern Italian Ridge of the Musicians Seamounts province, northeast of Hawaii. Although most of the samples analyzed are generally altered, a few are fresh. The latter exhibits similar geochemical and isotopic characteristics to normal MORB (Mid-Ocean Ridge Basalts). There are systematic geochemical trends from hotspot to mid-ocean ridge in the province. Incompatible element and isotopic variations suggest that the flow field had at least two distinct parental magmas, one with higher and one with lower MgO concentrations. The two parental magmas could be related by a magma mixing model. The major and trace element modeling shows that the two parental magmas could not have been produced by different degrees of melting of a homogeneous mantle source, but they are consistent with melting of a generally depleted mantle containing variable volumes of embedded enriched heterogeneity enriched interbeds.; Chemical and isotopic data of the lava samples dredged in the southern Bach Ridge and the northern Italian Ridge of the Musicians Seamounts province, northeast of Hawaii. Although most of the samples analyzed are generally altered, a few are fresh. The latter exhibits similar geochemical and isotopic characteristics to normal MORB (Mid-Ocean Ridge Basalts). There are systematic geochemical trends from hotspot to mid-ocean ridge in the province. Incompatible element and isotopic variations suggest that the flow field had at least two distinct parental magmas, one with higher and one with lower MgO concentrations. The two parental magmas could be related by a magma mixing model. The major and trace element modeling shows that the two parental magmas could not have been produced by different degrees of melting of a homogeneous mantle source, but they are consistent with melting of a generally depleted mantle containing variable volumes of embedded enriched heterogeneity enriched interbeds. |
学科主题 | Limnology ; Oceanography |
URL标识 | 查看原文 |
语种 | 英语 |
WOS记录号 | WOS:000262669100020 |
公开日期 | 2010-12-24 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/5039] |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China 3.Univ Hawaii, Dept Geol & Geophys, Honolulu, HI 96822 USA |
推荐引用方式 GB/T 7714 | Li Chuanshun,Pan Yucheng,Li Anchun,et al. Geochemistry of the lava and its implications in Musicians Seamounts[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2008,26(4):459-468. |
APA | Li Chuanshun,Pan Yucheng,Li Anchun,&Batiza, Rodey.(2008).Geochemistry of the lava and its implications in Musicians Seamounts.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,26(4),459-468. |
MLA | Li Chuanshun,et al."Geochemistry of the lava and its implications in Musicians Seamounts".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 26.4(2008):459-468. |
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